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overflow: hidden; text-overflow: ellipsis; -webkit-line-clamp: 3; -webkit-box-orient: vertical; }</style><div class="col-xs-12 clearfix"><div class="u-floatLeft"><h1 class="PageHeader-title u-m0x u-fs30">Shoreline Management Planning</h1><div class="u-tcGrayDark">1,414 Followers</div><div class="u-tcGrayDark u-mt2x">Recent papers in <b>Shoreline Management Planning</b></div></div></div></div></div></div><div class="TabbedNavigation"><div class="container"><div class="row"><div class="col-xs-12 clearfix"><ul class="nav u-m0x u-p0x list-inline u-displayFlex"><li class="active"><a href="https://www.academia.edu/Documents/in/Shoreline_Management_Planning">Top Papers</a></li><li><a href="https://www.academia.edu/Documents/in/Shoreline_Management_Planning/MostCited">Most Cited Papers</a></li><li><a href="https://www.academia.edu/Documents/in/Shoreline_Management_Planning/MostDownloaded">Most Downloaded Papers</a></li><li><a href="https://www.academia.edu/Documents/in/Shoreline_Management_Planning/MostRecent">Newest Papers</a></li><li><a class="" href="https://www.academia.edu/People/Shoreline_Management_Planning">People</a></li></ul></div><style type="text/css">ul.nav{flex-direction:row}@media(max-width: 567px){ul.nav{flex-direction:column}.TabbedNavigation li{max-width:100%}.TabbedNavigation li.active{background-color:var(--background-grey, #dddde2)}.TabbedNavigation li.active:before,.TabbedNavigation li.active:after{display:none}}</style></div></div></div><div class="container"><div class="row"><div class="col-xs-12"><div class="u-displayFlex"><div class="u-flexGrow1"><div class="works"><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_30928484" data-work_id="30928484" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/30928484/Near_Historical_Sea_Level_Rise_on_Sapelo_Island_Georgia">Near-Historical Sea Level Rise on Sapelo Island, Georgia</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Natural and anthropogenic climate changes, specifically from sea-level rise, are drastically reshaping coastal waterways and shorelines. However, few regional predictive models capture the longitudinal minutiae of hyper-local changes. In... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_30928484" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Natural and anthropogenic climate changes, specifically from sea-level rise, are drastically reshaping coastal waterways and shorelines. However, few regional predictive models capture the longitudinal minutiae of hyper-local changes. In response, I combined georeferenced maps from 1868-2015 with DEM and LiDAR data to calculate the rate of change at high-risk areas of Sapelo Island, Georgia through transect-based digital surveys. Geospatial  analyses are groundtruthed to: (1) test if climate changes are occurring at an increasingly rapid rate from 1860s- present; (2) calculate rate of change at site-specific scale; and (3) propose a triage system to identify, document, and mitigate at-risk cultural resources.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/30928484" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="17eb89d3049b093a2f8a300bbd12f903" rel="nofollow" data-download="{"attachment_id":51354579,"asset_id":30928484,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/51354579/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="933245" href="https://etsu.academia.edu/LindseyCochran">Lindsey Cochran</a><script data-card-contents-for-user="933245" type="text/json">{"id":933245,"first_name":"Lindsey","last_name":"Cochran","domain_name":"etsu","page_name":"LindseyCochran","display_name":"Lindsey Cochran","profile_url":"https://etsu.academia.edu/LindseyCochran?f_ri=43335","photo":"https://0.academia-photos.com/933245/883073/77988232/s65_lindsey.cochran.jpg"}</script></span></span></li><li class="js-paper-rank-work_30928484 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="30928484"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 30928484, container: ".js-paper-rank-work_30928484", }); 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However, few regional predictive models capture the longitudinal minutiae of hyper-local changes. In response, I combined georeferenced maps from 1868-2015 with DEM and LiDAR data to calculate the rate of change at high-risk areas of Sapelo Island, Georgia through transect-based digital surveys. Geospatial analyses are groundtruthed to: (1) test if climate changes are occurring at an increasingly rapid rate from 1860s- present; (2) calculate rate of change at site-specific scale; and (3) propose a triage system to identify, document, and mitigate at-risk cultural resources.","downloadable_attachments":[{"id":51354579,"asset_id":30928484,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":933245,"first_name":"Lindsey","last_name":"Cochran","domain_name":"etsu","page_name":"LindseyCochran","display_name":"Lindsey Cochran","profile_url":"https://etsu.academia.edu/LindseyCochran?f_ri=43335","photo":"https://0.academia-photos.com/933245/883073/77988232/s65_lindsey.cochran.jpg"}],"research_interests":[{"id":392,"name":"Archaeology","url":"https://www.academia.edu/Documents/in/Archaeology?f_ri=43335","nofollow":false},{"id":1512,"name":"Climate Change","url":"https://www.academia.edu/Documents/in/Climate_Change?f_ri=43335","nofollow":false},{"id":16723,"name":"Climate Change Adaptation And Mitigation Strategies","url":"https://www.academia.edu/Documents/in/Climate_Change_Adaptation_And_Mitigation_Strategies?f_ri=43335","nofollow":false},{"id":19522,"name":"Remote sensing and GIS applications in Landscape Research","url":"https://www.academia.edu/Documents/in/Remote_sensing_and_GIS_applications_in_Landscape_Research?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335"},{"id":443711,"name":"Gullah/Geechee Culture of the Lowcountry","url":"https://www.academia.edu/Documents/in/Gullah_Geechee_Culture_of_the_Lowcountry?f_ri=43335"},{"id":1009312,"name":"Geographic Information Systems (GIS)","url":"https://www.academia.edu/Documents/in/Geographic_Information_Systems_GIS_?f_ri=43335"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_6137899" data-work_id="6137899" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/6137899/Shoreline_Change_Evaluation_to_Improve_Spatial_Planning_In_Waterfront_Cities_Case_Study_Surabaya_Indonesia">Shoreline Change Evaluation to Improve Spatial Planning In Waterfront Cities. Case Study: Surabaya-Indonesia</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/6137899" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="c583bb15ecdcc13a9095bb5bee465a76" rel="nofollow" data-download="{"attachment_id":33035288,"asset_id":6137899,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/33035288/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="4655435" href="https://its.academia.edu/pratomoatmojo">Nursakti Adhi Pratomoatmojo</a><script data-card-contents-for-user="4655435" type="text/json">{"id":4655435,"first_name":"Nursakti Adhi","last_name":"Pratomoatmojo","domain_name":"its","page_name":"pratomoatmojo","display_name":"Nursakti Adhi Pratomoatmojo","profile_url":"https://its.academia.edu/pratomoatmojo?f_ri=43335","photo":"https://0.academia-photos.com/4655435/1953550/2309887/s65_nursakti.pratomoatmojo.jpg"}</script></span></span></li><li class="js-paper-rank-work_6137899 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="6137899"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 6137899, container: ".js-paper-rank-work_6137899", }); 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$(".js-view-count[data-work-id=6137899]").text(description); $(".js-view-count-work_6137899").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_6137899").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="6137899"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">2</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="28131" href="https://www.academia.edu/Documents/in/Urban_Waterfronts">Urban Waterfronts</a>, <script data-card-contents-for-ri="28131" type="text/json">{"id":28131,"name":"Urban Waterfronts","url":"https://www.academia.edu/Documents/in/Urban_Waterfronts?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="43335" href="https://www.academia.edu/Documents/in/Shoreline_Management_Planning">Shoreline Management Planning</a><script data-card-contents-for-ri="43335" type="text/json">{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=6137899]'), work: {"id":6137899,"title":"Shoreline Change Evaluation to Improve Spatial Planning In Waterfront Cities. Case Study: Surabaya-Indonesia","created_at":"2014-02-19T13:09:42.134-08:00","url":"https://www.academia.edu/6137899/Shoreline_Change_Evaluation_to_Improve_Spatial_Planning_In_Waterfront_Cities_Case_Study_Surabaya_Indonesia?f_ri=43335","dom_id":"work_6137899","summary":null,"downloadable_attachments":[{"id":33035288,"asset_id":6137899,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":4655435,"first_name":"Nursakti Adhi","last_name":"Pratomoatmojo","domain_name":"its","page_name":"pratomoatmojo","display_name":"Nursakti Adhi Pratomoatmojo","profile_url":"https://its.academia.edu/pratomoatmojo?f_ri=43335","photo":"https://0.academia-photos.com/4655435/1953550/2309887/s65_nursakti.pratomoatmojo.jpg"}],"research_interests":[{"id":28131,"name":"Urban Waterfronts","url":"https://www.academia.edu/Documents/in/Urban_Waterfronts?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_15711391" data-work_id="15711391" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/15711391/An_Integrated_Study_on_the_Impact_of_Anthropogenic_Influenced_Coastal_Erosion_in_Puducherry_and_Villupuram_Coasts_Bay_of_Bengal_South_India">An Integrated Study on the Impact of Anthropogenic Influenced Coastal Erosion in Puducherry and Villupuram Coasts, Bay of Bengal, South India</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">This paper focuses on shoreline changes due to erosion in the Puducherry coast of southern peninsular region in India. Accurate detection and frequent monitoring of shorelines are very essential to understand the coastal processes and its... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_15711391" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">This paper focuses on shoreline changes due to erosion in the Puducherry coast of southern peninsular region in India. Accurate detection and frequent monitoring of shorelines are very essential to understand the coastal processes and its impact on coastal zone habitats. The present study is to investigate the spatial as well as quantify the shoreline erosion and accretion along the coast in the parts of Puducherry state and Villupuram district, east coast of Tamil Nadu by using geospatial techniques. The Survey of India topographic map, multi-temporal Remote Sensing satellite data were used to extract the shorelines. The data is processed and analyzed by software like ENVI image processing, Qgis and ArcGIS respectively. The rates of shoreline changes are estimated by Digital Shoreline Analysis System (DSAS) using GIS environment. Due to length of the shoreline, the study area has divided into four segments namely A, B, C and D. The study reveals that most of the study area has been undergoing erosion around 289m for the past 30 decades except south most part of Segment D. Both natural and anthropogenic processes along the coast modify the shoreline configuration and control the erosion, accretion activities of the coastal zones.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/15711391" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="cce0418e049f1c3ab610a85ddcf507de" rel="nofollow" data-download="{"attachment_id":38772522,"asset_id":15711391,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/38772522/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="7199497" href="https://alagappauniversity.academia.edu/SivakumarKarthikeyan">Sivakumar Karthikeyan</a><script data-card-contents-for-user="7199497" type="text/json">{"id":7199497,"first_name":"Sivakumar","last_name":"Karthikeyan","domain_name":"alagappauniversity","page_name":"SivakumarKarthikeyan","display_name":"Sivakumar Karthikeyan","profile_url":"https://alagappauniversity.academia.edu/SivakumarKarthikeyan?f_ri=43335","photo":"https://0.academia-photos.com/7199497/3921600/24443033/s65_sivakumar.karthikeyan.jpg"}</script></span></span></li><li class="js-paper-rank-work_15711391 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="15711391"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 15711391, container: ".js-paper-rank-work_15711391", }); 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$(".js-view-count[data-work-id=15711391]").text(description); $(".js-view-count-work_15711391").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_15711391").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="15711391"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">6</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="23408" href="https://www.academia.edu/Documents/in/Remote_sensing_and_GIS">Remote sensing and GIS</a>, <script data-card-contents-for-ri="23408" type="text/json">{"id":23408,"name":"Remote sensing and GIS","url":"https://www.academia.edu/Documents/in/Remote_sensing_and_GIS?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="40021" href="https://www.academia.edu/Documents/in/Coastal_Zone_Management">Coastal Zone Management</a>, <script data-card-contents-for-ri="40021" type="text/json">{"id":40021,"name":"Coastal Zone Management","url":"https://www.academia.edu/Documents/in/Coastal_Zone_Management?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="43335" href="https://www.academia.edu/Documents/in/Shoreline_Management_Planning">Shoreline Management Planning</a>, <script data-card-contents-for-ri="43335" type="text/json">{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="87756" href="https://www.academia.edu/Documents/in/Integrated_Coastal_Zone_Management">Integrated Coastal Zone Management</a><script data-card-contents-for-ri="87756" type="text/json">{"id":87756,"name":"Integrated Coastal Zone Management","url":"https://www.academia.edu/Documents/in/Integrated_Coastal_Zone_Management?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=15711391]'), work: {"id":15711391,"title":"An Integrated Study on the Impact of Anthropogenic Influenced Coastal Erosion in Puducherry and Villupuram Coasts, Bay of Bengal, South India","created_at":"2015-09-14T23:56:24.490-07:00","url":"https://www.academia.edu/15711391/An_Integrated_Study_on_the_Impact_of_Anthropogenic_Influenced_Coastal_Erosion_in_Puducherry_and_Villupuram_Coasts_Bay_of_Bengal_South_India?f_ri=43335","dom_id":"work_15711391","summary":"This paper focuses on shoreline changes due to erosion in the Puducherry coast of southern peninsular region in India. Accurate detection and frequent monitoring of shorelines are very essential to understand the coastal processes and its impact on coastal zone habitats. The present study is to investigate the spatial as well as quantify the shoreline erosion and accretion along the coast in the parts of Puducherry state and Villupuram district, east coast of Tamil Nadu by using geospatial techniques. The Survey of India topographic map, multi-temporal Remote Sensing satellite data were used to extract the shorelines. The data is processed and analyzed by software like ENVI image processing, Qgis and ArcGIS respectively. The rates of shoreline changes are estimated by Digital Shoreline Analysis System (DSAS) using GIS environment. Due to length of the shoreline, the study area has divided into four segments namely A, B, C and D. The study reveals that most of the study area has been undergoing erosion around 289m for the past 30 decades except south most part of Segment D. Both natural and anthropogenic processes along the coast modify the shoreline configuration and control the erosion, accretion activities of the coastal zones.","downloadable_attachments":[{"id":38772522,"asset_id":15711391,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":7199497,"first_name":"Sivakumar","last_name":"Karthikeyan","domain_name":"alagappauniversity","page_name":"SivakumarKarthikeyan","display_name":"Sivakumar Karthikeyan","profile_url":"https://alagappauniversity.academia.edu/SivakumarKarthikeyan?f_ri=43335","photo":"https://0.academia-photos.com/7199497/3921600/24443033/s65_sivakumar.karthikeyan.jpg"}],"research_interests":[{"id":23408,"name":"Remote sensing and GIS","url":"https://www.academia.edu/Documents/in/Remote_sensing_and_GIS?f_ri=43335","nofollow":false},{"id":40021,"name":"Coastal Zone Management","url":"https://www.academia.edu/Documents/in/Coastal_Zone_Management?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false},{"id":87756,"name":"Integrated Coastal Zone Management","url":"https://www.academia.edu/Documents/in/Integrated_Coastal_Zone_Management?f_ri=43335","nofollow":false},{"id":440716,"name":"Remote Sensing for Shoreline Change","url":"https://www.academia.edu/Documents/in/Remote_Sensing_for_Shoreline_Change?f_ri=43335"},{"id":1155016,"name":"Shoreline Mapping","url":"https://www.academia.edu/Documents/in/Shoreline_Mapping?f_ri=43335"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_9094497 coauthored" data-work_id="9094497" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/9094497/Human_influence_and_the_changing_geomorphology_of_Mediterranean_deltas">Human influence and the changing geomorphology of Mediterranean deltas</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The present geomorphology of the Mediterranean’s coasts is largely a product of an intricate long-term relationship between Nature and human societies. A cradle of ancient civilizations, the Mediterranean has seen its shores occupied by... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_9094497" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The present geomorphology of the Mediterranean’s coasts is largely a product of an intricate long-term relationship between Nature and human societies. A cradle of ancient <br />civilizations, the Mediterranean has seen its shores occupied by Humans since Prehistory, and is, therefore, a particularly pertinent unit of analysis. The morphotectonic context and <br />other forcing agents (e.g., climate) shaped out a highly diversified coastal morphology and generated a sediment-supply regime potentially favourable to the formation of numerous open-coast deltas and bay-head deltas in infilled rias as sea level stabilised during the mid- Holocene. This supply of riverine sediment has also been the key agent in mediating human occupation of the Mediterranean’s clastic coasts. <br /> <br />Expressions of this relationship have been extensively archived in clastic coastal deposits, including base-level deltaic and estuarine sedimentary sinks, which comprise records to explore the interactions between geosystemsand the human environment. The stratigraphic sequences in these coastal sedimentary archives comprise, in many places, a clearly identified anthropogenic signature, notably in ancient harbours, some of which underwent extremely rapid silting up due to massive sediment sourcing generated by new agricultural practices from the Neolithic onwards. <br /> <br />Increasing human influence, especially over the last 3000 years, has been, in turn, an important driver of changes in sediment supply, strongly modulating deltaic development. <br />Pulses of sediment supply from catchments rendered vulnerable by human perturbations during the Roman period resulted in a new cycle of inception of many other deltas and in <br />rapid delta growth (e.g. the Ebro, the Po, the Arno and the Ombrone). Another progradation dynamic during the Little Ice Age, at a time of strong rural population growth, river discharge <br />increases, technological developments, and urbanisation, further consolidated delta growth. <br /> <br />Understanding the life cycle of these deltas since their initial formation is, in turn, key to unravelling the relative role of natural and anthropogenic forcing agents. Rapid climate <br />changes are deemed to have contributed through both the stripping of landscapes rendered fragile by human activities and active fluvial sediment transport to the coast, but <br />disentangling climate change effects from human impacts in the Mediterranean remains a challenge. <br /> <br />The patterns of subsequent deltaic growth and delta morphodynamics reflect adaptations to pulsed sediment supply, river discharge variations, the microtidal, fetchlimited <br />context of the Mediterranean, and direct engineering interventions. The progradation dynamic of the Roman period and Little Ice Age contrasts markedly with the situation of common coastal destabilisation over the last two centuries, particularly well documented for the last 50 years. This period has been characterised by reduced sediment flux to base-level geosystems due to catchment reforestation, retenion within reservoirs, fluvial regulation and dredging, resulting in the erosion of deltas and barrier-lagoon and beach-dune systems. Large stretches of shoreline and narrow coastal plains have been massively engineered for coastal defence and protection against erosion, but also for the construction of marinas, leisure harbours and artificial beaches, resulting in the emergence of veritable artificial seafronts. These interventions have, collectively and progressively, raised societies to a pervasive and overarching position in the geomorphic stabilityinstability of the Mediterranean’s coasts, a situation that will be exacerbated by pressures from sea-level rise, paving the way for rampant coastal erosion and delta destruction.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/9094497" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="4e33473c9835686e1cda3c2087bbe575" rel="nofollow" data-download="{"attachment_id":35439543,"asset_id":9094497,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/35439543/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="514788" href="https://univ-amu.academia.edu/ChristopheMorhange">Christophe Morhange</a><script data-card-contents-for-user="514788" type="text/json">{"id":514788,"first_name":"Christophe","last_name":"Morhange","domain_name":"univ-amu","page_name":"ChristopheMorhange","display_name":"Christophe Morhange","profile_url":"https://univ-amu.academia.edu/ChristopheMorhange?f_ri=43335","photo":"https://0.academia-photos.com/514788/213655/249510/s65_christophe.morhange.jpg"}</script></span></span><span class="u-displayInlineBlock InlineList-item-text"> and <span class="u-textDecorationUnderline u-clickable InlineList-item-text js-work-more-authors-9094497">+1</span><div class="hidden js-additional-users-9094497"><div><span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a href="https://cnrs.academia.edu/NickMarriner">Nick Marriner</a></span></div></div></span><script>(function(){ var popoverSettings = { el: $('.js-work-more-authors-9094497'), placement: 'bottom', hide_delay: 200, html: true, content: function(){ return $('.js-additional-users-9094497').html(); } } new HoverPopover(popoverSettings); })();</script></li><li class="js-paper-rank-work_9094497 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="9094497"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 9094497, container: ".js-paper-rank-work_9094497", }); });</script></li><li class="js-percentile-work_9094497 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 9094497; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_9094497"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_9094497 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="9094497"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 9094497; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=9094497]").text(description); $(".js-view-count-work_9094497").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_9094497").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="9094497"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">44</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="153" href="https://www.academia.edu/Documents/in/Landscape_Ecology">Landscape Ecology</a>, <script data-card-contents-for-ri="153" type="text/json">{"id":153,"name":"Landscape Ecology","url":"https://www.academia.edu/Documents/in/Landscape_Ecology?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="261" href="https://www.academia.edu/Documents/in/Geography">Geography</a>, <script data-card-contents-for-ri="261" type="text/json">{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="392" href="https://www.academia.edu/Documents/in/Archaeology">Archaeology</a>, <script data-card-contents-for-ri="392" type="text/json">{"id":392,"name":"Archaeology","url":"https://www.academia.edu/Documents/in/Archaeology?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="396" href="https://www.academia.edu/Documents/in/Maritime_Archaeology">Maritime Archaeology</a><script data-card-contents-for-ri="396" type="text/json">{"id":396,"name":"Maritime Archaeology","url":"https://www.academia.edu/Documents/in/Maritime_Archaeology?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=9094497]'), work: {"id":9094497,"title":"Human influence and the changing geomorphology of Mediterranean deltas","created_at":"2014-11-03T00:35:58.838-08:00","url":"https://www.academia.edu/9094497/Human_influence_and_the_changing_geomorphology_of_Mediterranean_deltas?f_ri=43335","dom_id":"work_9094497","summary":"The present geomorphology of the Mediterranean’s coasts is largely a product of an intricate long-term relationship between Nature and human societies. A cradle of ancient\r\ncivilizations, the Mediterranean has seen its shores occupied by Humans since Prehistory, and is, therefore, a particularly pertinent unit of analysis. The morphotectonic context and\r\nother forcing agents (e.g., climate) shaped out a highly diversified coastal morphology and generated a sediment-supply regime potentially favourable to the formation of numerous open-coast deltas and bay-head deltas in infilled rias as sea level stabilised during the mid- Holocene. This supply of riverine sediment has also been the key agent in mediating human occupation of the Mediterranean’s clastic coasts. \r\n\r\nExpressions of this relationship have been extensively archived in clastic coastal deposits, including base-level deltaic and estuarine sedimentary sinks, which comprise records to explore the interactions between geosystemsand the human environment. The stratigraphic sequences in these coastal sedimentary archives comprise, in many places, a clearly identified anthropogenic signature, notably in ancient harbours, some of which underwent extremely rapid silting up due to massive sediment sourcing generated by new agricultural practices from the Neolithic onwards.\r\n\r\nIncreasing human influence, especially over the last 3000 years, has been, in turn, an important driver of changes in sediment supply, strongly modulating deltaic development.\r\nPulses of sediment supply from catchments rendered vulnerable by human perturbations during the Roman period resulted in a new cycle of inception of many other deltas and in\r\nrapid delta growth (e.g. the Ebro, the Po, the Arno and the Ombrone). Another progradation dynamic during the Little Ice Age, at a time of strong rural population growth, river discharge\r\nincreases, technological developments, and urbanisation, further consolidated delta growth.\r\n\r\nUnderstanding the life cycle of these deltas since their initial formation is, in turn, key to unravelling the relative role of natural and anthropogenic forcing agents. Rapid climate\r\nchanges are deemed to have contributed through both the stripping of landscapes rendered fragile by human activities and active fluvial sediment transport to the coast, but\r\ndisentangling climate change effects from human impacts in the Mediterranean remains a challenge.\r\n\r\nThe patterns of subsequent deltaic growth and delta morphodynamics reflect adaptations to pulsed sediment supply, river discharge variations, the microtidal, fetchlimited\r\ncontext of the Mediterranean, and direct engineering interventions. The progradation dynamic of the Roman period and Little Ice Age contrasts markedly with the situation of common coastal destabilisation over the last two centuries, particularly well documented for the last 50 years. This period has been characterised by reduced sediment flux to base-level geosystems due to catchment reforestation, retenion within reservoirs, fluvial regulation and dredging, resulting in the erosion of deltas and barrier-lagoon and beach-dune systems. Large stretches of shoreline and narrow coastal plains have been massively engineered for coastal defence and protection against erosion, but also for the construction of marinas, leisure harbours and artificial beaches, resulting in the emergence of veritable artificial seafronts. These interventions have, collectively and progressively, raised societies to a pervasive and overarching position in the geomorphic stabilityinstability of the Mediterranean’s coasts, a situation that will be exacerbated by pressures from sea-level rise, paving the way for rampant coastal erosion and delta destruction.","downloadable_attachments":[{"id":35439543,"asset_id":9094497,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":514788,"first_name":"Christophe","last_name":"Morhange","domain_name":"univ-amu","page_name":"ChristopheMorhange","display_name":"Christophe Morhange","profile_url":"https://univ-amu.academia.edu/ChristopheMorhange?f_ri=43335","photo":"https://0.academia-photos.com/514788/213655/249510/s65_christophe.morhange.jpg"},{"id":905185,"first_name":"Nick","last_name":"Marriner","domain_name":"cnrs","page_name":"NickMarriner","display_name":"Nick Marriner","profile_url":"https://cnrs.academia.edu/NickMarriner?f_ri=43335","photo":"https://0.academia-photos.com/905185/18291379/18260239/s65_nick.marriner.jpg"}],"research_interests":[{"id":153,"name":"Landscape Ecology","url":"https://www.academia.edu/Documents/in/Landscape_Ecology?f_ri=43335","nofollow":false},{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography?f_ri=43335","nofollow":false},{"id":392,"name":"Archaeology","url":"https://www.academia.edu/Documents/in/Archaeology?f_ri=43335","nofollow":false},{"id":396,"name":"Maritime Archaeology","url":"https://www.academia.edu/Documents/in/Maritime_Archaeology?f_ri=43335","nofollow":false},{"id":399,"name":"Prehistoric Archaeology","url":"https://www.academia.edu/Documents/in/Prehistoric_Archaeology?f_ri=43335"},{"id":408,"name":"Geomorphology","url":"https://www.academia.edu/Documents/in/Geomorphology?f_ri=43335"},{"id":1275,"name":"Coastal 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Archaeology","url":"https://www.academia.edu/Documents/in/Islands_Archaeology?f_ri=43335"},{"id":1650018,"name":"Human Influence","url":"https://www.academia.edu/Documents/in/Human_Influence?f_ri=43335"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_6160291" data-work_id="6160291" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/6160291/Des_plages_dans_la_ville_Los_Angeles_et_la_r%C3%A9flexion_sur_la_plage_urbaine_id%C3%A9ale">Des plages dans la ville : Los Angeles et la réflexion sur la plage urbaine idéale</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button 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data-card-contents-for-ri="3722" type="text/json">{"id":3722,"name":"Environmental History","url":"https://www.academia.edu/Documents/in/Environmental_History?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="43335" href="https://www.academia.edu/Documents/in/Shoreline_Management_Planning">Shoreline Management Planning</a>, <script data-card-contents-for-ri="43335" type="text/json">{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="43390" href="https://www.academia.edu/Documents/in/Sandy_Beaches">Sandy Beaches</a><script data-card-contents-for-ri="43390" type="text/json">{"id":43390,"name":"Sandy Beaches","url":"https://www.academia.edu/Documents/in/Sandy_Beaches?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=6160291]'), work: {"id":6160291,"title":"Des plages dans la ville : Los Angeles et la réflexion sur la plage urbaine idéale","created_at":"2014-02-21T05:38:20.600-08:00","url":"https://www.academia.edu/6160291/Des_plages_dans_la_ville_Los_Angeles_et_la_r%C3%A9flexion_sur_la_plage_urbaine_id%C3%A9ale?f_ri=43335","dom_id":"work_6160291","summary":null,"downloadable_attachments":[{"id":33049541,"asset_id":6160291,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":9366648,"first_name":"Elsa","last_name":"Devienne","domain_name":"northumbria","page_name":"ElsaDevienne","display_name":"Elsa Devienne","profile_url":"https://northumbria.academia.edu/ElsaDevienne?f_ri=43335","photo":"https://0.academia-photos.com/9366648/2990866/11141699/s65_elsa.devienne.jpg"}],"research_interests":[{"id":3722,"name":"Environmental History","url":"https://www.academia.edu/Documents/in/Environmental_History?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false},{"id":43390,"name":"Sandy Beaches","url":"https://www.academia.edu/Documents/in/Sandy_Beaches?f_ri=43335","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_34320405" data-work_id="34320405" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/34320405/Shoreline_change_assessment_using_multi_temporal_satellite_images_a_case_study_of_Lake_Sapanca_NW_Turkey">Shoreline change assessment using multi-temporal satellite images: a case study of Lake Sapanca, NW Turkey</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The research summarized here determines historical shoreline changes along Lake Sapanca by using Remote Sensing (RS) and Geographical Information Systems (GIS). Six multi-temporal satellite images of Landsat Multispectral Scanner (L1-5... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_34320405" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The research summarized here determines historical shoreline changes along Lake Sapanca by using Remote Sensing (RS) and Geographical Information Systems (GIS). Six multi-temporal satellite images of Landsat Multispectral Scanner (L1-5 MMS), Enhanced Thematic Mapper Plus (L7 ETM+), and Operational Land Imager Sensors (L8 OLI), covering the period between 17 June 1975 and 15 July 2016, were used to monitor shoreline positions and estimate change rates along the coastal zone. After pre-possessing routines, the Normalized Difference Water Index (NDWI), Modified Normalized Difference Water Index (MNDWI), and supervised classification techniques were utilized to extract six different shorelines. Digital Shoreline Analysis System (DSAS), a toolbox that enables transect-based computations of shoreline displacement, was used to compute historical shoreline change rates. The average rate of shoreline change for the entire cost was 2.7 m/year of progradation with an uncertainty of 0.2 m/year. While the great part of the lake shoreline remained stable, the study concluded that the easterly and westerly coasts and deltaic coasts are more vulnerable to shoreline displacements over the last four decades. The study also reveals that anthropogenic activities, more specifically over extraction of freshwater from the lake, cyclic variation in rainfall, and deposition of sediment transported by the surrounding creeks dominantly control spatiotemporal shoreline changes in the region. Monitoring shoreline changes using multi-temporal satellite images is a significant component for the coastal decision-making and management.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/34320405" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="8576414d5fc8f2b1f29316a75d60a48d" rel="nofollow" data-download="{"attachment_id":54219367,"asset_id":34320405,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/54219367/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="36499235" href="https://independent.academia.edu/UmitDuru">Umit Duru</a><script data-card-contents-for-user="36499235" type="text/json">{"id":36499235,"first_name":"Umit","last_name":"Duru","domain_name":"independent","page_name":"UmitDuru","display_name":"Umit Duru","profile_url":"https://independent.academia.edu/UmitDuru?f_ri=43335","photo":"https://0.academia-photos.com/36499235/17561991/20913516/s65_umit.duru.jpg"}</script></span></span></li><li class="js-paper-rank-work_34320405 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="34320405"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 34320405, container: ".js-paper-rank-work_34320405", }); 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Six multi-temporal satellite images of Landsat Multispectral Scanner (L1-5 MMS), Enhanced Thematic Mapper Plus (L7 ETM+), and Operational Land Imager Sensors (L8 OLI), covering the period between 17 June 1975 and 15 July 2016, were used to monitor shoreline positions and estimate change rates along the coastal zone. After pre-possessing routines, the Normalized Difference Water Index (NDWI), Modified Normalized Difference Water Index (MNDWI), and supervised classification techniques were utilized to extract six different shorelines. Digital Shoreline Analysis System (DSAS), a toolbox that enables transect-based computations of shoreline displacement, was used to compute historical shoreline change rates. The average rate of shoreline change for the entire cost was 2.7 m/year of progradation with an uncertainty of 0.2 m/year. While the great part of the lake shoreline remained stable, the study concluded that the easterly and westerly coasts and deltaic coasts are more vulnerable to shoreline displacements over the last four decades. The study also reveals that anthropogenic activities, more specifically over extraction of freshwater from the lake, cyclic variation in rainfall, and deposition of sediment transported by the surrounding creeks dominantly control spatiotemporal shoreline changes in the region. Monitoring shoreline changes using multi-temporal satellite images is a significant component for the coastal decision-making and management.","downloadable_attachments":[{"id":54219367,"asset_id":34320405,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":36499235,"first_name":"Umit","last_name":"Duru","domain_name":"independent","page_name":"UmitDuru","display_name":"Umit Duru","profile_url":"https://independent.academia.edu/UmitDuru?f_ri=43335","photo":"https://0.academia-photos.com/36499235/17561991/20913516/s65_umit.duru.jpg"}],"research_interests":[{"id":6808,"name":"Coastal Geomorphology","url":"https://www.academia.edu/Documents/in/Coastal_Geomorphology?f_ri=43335","nofollow":false},{"id":23408,"name":"Remote sensing and GIS","url":"https://www.academia.edu/Documents/in/Remote_sensing_and_GIS?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_727079" data-work_id="727079" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/727079/The_Italian_Data_Buoy_Network">The Italian Data Buoy Network</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The Italian Data Buoy Network consists of 15 oceanographic buoys, deployed along Italian coasts, on a seabed 100 meters deep. It collects directional sea wave data, meteorological data, sea surface temperature and in some cases quality... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_727079" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The Italian Data Buoy Network consists of 15 oceanographic buoys, deployed along Italian coasts, on a seabed 100 meters deep. It collects directional sea wave data, meteorological data, sea surface temperature and in some cases quality parameters. Acoustic Doppler Current Profilers (ADCP) and hyperspectral<br />probes will be added in the future. The network will be also the main framework for tsunami wave study in the central Mediterranean Sea, and an early technological platform to study low-frequency sea motion detected in open sea using high-precision, multichannel, multisatellite GPS/Glonass/Galileo receivers and sea bottom instrumentation equipped with nano-resolution pressure sensors.<br /><br />Keywords: Data buoys, coastal management, directional wave measurement, gravity waves, physical oceanography, iSSH, SST, tide, tidal waves, tsunami.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/727079" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="de8f0925a3fcb30cbf5dc1aa61b72691" rel="nofollow" data-download="{"attachment_id":4139549,"asset_id":727079,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/4139549/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="538132" href="https://independent.academia.edu/FurioRuggiero">Furio Ruggiero</a><script data-card-contents-for-user="538132" type="text/json">{"id":538132,"first_name":"Furio","last_name":"Ruggiero","domain_name":"independent","page_name":"FurioRuggiero","display_name":"Furio Ruggiero","profile_url":"https://independent.academia.edu/FurioRuggiero?f_ri=43335","photo":"https://0.academia-photos.com/538132/192693/392066/s65_furio.ruggiero.jpg"}</script></span></span></li><li class="js-paper-rank-work_727079 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="727079"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 727079, container: ".js-paper-rank-work_727079", }); });</script></li><li class="js-percentile-work_727079 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 727079; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_727079"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_727079 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="727079"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 727079; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=727079]").text(description); $(".js-view-count-work_727079").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_727079").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="727079"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">7</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="81" href="https://www.academia.edu/Documents/in/Ocean_Engineering">Ocean Engineering</a>, <script data-card-contents-for-ri="81" type="text/json">{"id":81,"name":"Ocean Engineering","url":"https://www.academia.edu/Documents/in/Ocean_Engineering?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="16691" href="https://www.academia.edu/Documents/in/Physical_Oceanography">Physical Oceanography</a>, <script data-card-contents-for-ri="16691" type="text/json">{"id":16691,"name":"Physical Oceanography","url":"https://www.academia.edu/Documents/in/Physical_Oceanography?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="20051" href="https://www.academia.edu/Documents/in/Biological_Oceanography">Biological Oceanography</a>, <script data-card-contents-for-ri="20051" type="text/json">{"id":20051,"name":"Biological Oceanography","url":"https://www.academia.edu/Documents/in/Biological_Oceanography?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="27085" href="https://www.academia.edu/Documents/in/Tsunami">Tsunami</a><script data-card-contents-for-ri="27085" type="text/json">{"id":27085,"name":"Tsunami","url":"https://www.academia.edu/Documents/in/Tsunami?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=727079]'), work: {"id":727079,"title":"The Italian Data Buoy Network","created_at":"2011-07-08T20:43:59.911-07:00","url":"https://www.academia.edu/727079/The_Italian_Data_Buoy_Network?f_ri=43335","dom_id":"work_727079","summary":"The Italian Data Buoy Network consists of 15 oceanographic buoys, deployed along Italian coasts, on a seabed 100 meters deep. It collects directional sea wave data, meteorological data, sea surface temperature and in some cases quality parameters. Acoustic Doppler Current Profilers (ADCP) and hyperspectral\nprobes will be added in the future. The network will be also the main framework for tsunami wave study in the central Mediterranean Sea, and an early technological platform to study low-frequency sea motion detected in open sea using high-precision, multichannel, multisatellite GPS/Glonass/Galileo receivers and sea bottom instrumentation equipped with nano-resolution pressure sensors.\n\nKeywords: Data buoys, coastal management, directional wave measurement, gravity waves, physical oceanography, iSSH, SST, tide, tidal waves, tsunami.","downloadable_attachments":[{"id":4139549,"asset_id":727079,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":538132,"first_name":"Furio","last_name":"Ruggiero","domain_name":"independent","page_name":"FurioRuggiero","display_name":"Furio Ruggiero","profile_url":"https://independent.academia.edu/FurioRuggiero?f_ri=43335","photo":"https://0.academia-photos.com/538132/192693/392066/s65_furio.ruggiero.jpg"}],"research_interests":[{"id":81,"name":"Ocean Engineering","url":"https://www.academia.edu/Documents/in/Ocean_Engineering?f_ri=43335","nofollow":false},{"id":16691,"name":"Physical Oceanography","url":"https://www.academia.edu/Documents/in/Physical_Oceanography?f_ri=43335","nofollow":false},{"id":20051,"name":"Biological Oceanography","url":"https://www.academia.edu/Documents/in/Biological_Oceanography?f_ri=43335","nofollow":false},{"id":27085,"name":"Tsunami","url":"https://www.academia.edu/Documents/in/Tsunami?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335"},{"id":61634,"name":"Environmentally Shore Protection","url":"https://www.academia.edu/Documents/in/Environmentally_Shore_Protection?f_ri=43335"},{"id":84109,"name":"Tsunamigenic Earthquakes","url":"https://www.academia.edu/Documents/in/Tsunamigenic_Earthquakes?f_ri=43335"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_40217701" data-work_id="40217701" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/40217701/Dynamics_of_coastline_changes_in_Mexico">Dynamics of coastline changes in Mexico</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The goal of our work was to locate and quantify changes that occurred in 66% of the Mexican coastline, based on four land cover maps generated by the Mexican Mangrove Monitoring System (SMMM) of the National Commission for the Knowledge... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_40217701" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The goal of our work was to locate and quantify changes that occurred in 66% of the Mexican coastline, based on four land cover maps generated by the Mexican Mangrove Monitoring System (SMMM) of the National Commission for the Knowledge and Use of Biodiversity (CONABIO) for the years 1970/81, 2005, 2010, and 2015. Our results showed overall dominance of erosion over accretion processes, beaches being the most affected coastal land cover. Emphasis was placed on identification and description of coastline sites in which land was either continuously lost (erosion) or gained (accretion) during the studied time periods. These sites were defined as continuous unidirectional dynamic sites and were compared with previous knowledge about the geodynamics of Mexican coasts. Continuous unidirectional dynamic sites were distributed throughout the study area and within all land cover types, but predominantly corresponded to areas covered by mangroves in the states of Campeche and Nayarit. Finally, we found an intensification of coastal erosion-accretion processes over time; coastline change rates having duplicated between the earliest (1970/81-2005) and the two more recent (2005-2010, and 2010-2015) analysed time periods , with erosion rates for each corresponding period of-3 m/yr,-7.5 m/yr, and-7.3 m/yr, and accretion rates of 2.8 m/yr, 7.3 m/yr, and 6.9 m/yr, respectively.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/40217701" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="d90670efea039cb9c88d22cf3bab2e22" rel="nofollow" data-download="{"attachment_id":60445766,"asset_id":40217701,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/60445766/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="32325558" href="https://uca-es.academia.edu/JuanMunozperez">Juan J Munoz-perez</a><script data-card-contents-for-user="32325558" type="text/json">{"id":32325558,"first_name":"Juan","last_name":"Munoz-perez","domain_name":"uca-es","page_name":"JuanMunozperez","display_name":"Juan J Munoz-perez","profile_url":"https://uca-es.academia.edu/JuanMunozperez?f_ri=43335","photo":"https://0.academia-photos.com/32325558/12866337/14263400/s65_juan.munoz-perez.jpg"}</script></span></span></li><li class="js-paper-rank-work_40217701 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="40217701"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 40217701, container: ".js-paper-rank-work_40217701", }); });</script></li><li class="js-percentile-work_40217701 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 40217701; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_40217701"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_40217701 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="40217701"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 40217701; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=40217701]").text(description); $(".js-view-count-work_40217701").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_40217701").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="40217701"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">2</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="27086" href="https://www.academia.edu/Documents/in/Coastal_Erosion">Coastal Erosion</a>, <script data-card-contents-for-ri="27086" type="text/json">{"id":27086,"name":"Coastal Erosion","url":"https://www.academia.edu/Documents/in/Coastal_Erosion?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="43335" href="https://www.academia.edu/Documents/in/Shoreline_Management_Planning">Shoreline Management Planning</a><script data-card-contents-for-ri="43335" type="text/json">{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=40217701]'), work: {"id":40217701,"title":"Dynamics of coastline changes in Mexico","created_at":"2019-08-31T02:00:25.442-07:00","url":"https://www.academia.edu/40217701/Dynamics_of_coastline_changes_in_Mexico?f_ri=43335","dom_id":"work_40217701","summary":"The goal of our work was to locate and quantify changes that occurred in 66% of the Mexican coastline, based on four land cover maps generated by the Mexican Mangrove Monitoring System (SMMM) of the National Commission for the Knowledge and Use of Biodiversity (CONABIO) for the years 1970/81, 2005, 2010, and 2015. Our results showed overall dominance of erosion over accretion processes, beaches being the most affected coastal land cover. Emphasis was placed on identification and description of coastline sites in which land was either continuously lost (erosion) or gained (accretion) during the studied time periods. These sites were defined as continuous unidirectional dynamic sites and were compared with previous knowledge about the geodynamics of Mexican coasts. Continuous unidirectional dynamic sites were distributed throughout the study area and within all land cover types, but predominantly corresponded to areas covered by mangroves in the states of Campeche and Nayarit. Finally, we found an intensification of coastal erosion-accretion processes over time; coastline change rates having duplicated between the earliest (1970/81-2005) and the two more recent (2005-2010, and 2010-2015) analysed time periods , with erosion rates for each corresponding period of-3 m/yr,-7.5 m/yr, and-7.3 m/yr, and accretion rates of 2.8 m/yr, 7.3 m/yr, and 6.9 m/yr, respectively.","downloadable_attachments":[{"id":60445766,"asset_id":40217701,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":32325558,"first_name":"Juan","last_name":"Munoz-perez","domain_name":"uca-es","page_name":"JuanMunozperez","display_name":"Juan J Munoz-perez","profile_url":"https://uca-es.academia.edu/JuanMunozperez?f_ri=43335","photo":"https://0.academia-photos.com/32325558/12866337/14263400/s65_juan.munoz-perez.jpg"}],"research_interests":[{"id":27086,"name":"Coastal Erosion","url":"https://www.academia.edu/Documents/in/Coastal_Erosion?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_44479108" data-work_id="44479108" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/44479108/Numerical_Modeling_of_Sediment_Transport_Rate_and_Shoreline_Changes_of_Jazireh_e_Shomali_Jonoubi_Port_in_the_Persian_Gulf">Numerical Modeling of Sediment Transport Rate and Shoreline Changes of Jazireh-e Shomali-Jonoubi Port in the Persian Gulf</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Studying the sediments and predicting the coastal morphological changes have wide applications in coastal engineering, including coastal management, operation, and design of the structures as well as their maintenance, development, and... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_44479108" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Studying the sediments and predicting the coastal morphological changes have wide applications in coastal engineering, including coastal management, operation, and design of the structures as well as their maintenance, development, and expansion of coasts and coastal structures, which are of paramount importance. The aims of this study are to model the shoreline changes around the Jazireh-e Shomali-Jonoubi Port, calculate the amount of advancement and recession due to the construction of the breakwater, and to determine the areas exposed to erosion and sedimentation. To this end, a series of primary information, including aerial and satellite images, hydrographic and topographic maps, and the specifications and grading of the sediment of the considered coast, has been collected and the overall morphology of the area has been determined. The input data into the model include a 12-year time series of the wave (height, period, and direction of the wave) and the wave climate. The length of the shoreline is 4 km and a profile perpendicular to the coast with a length of 1500 m has been applied to the model. Finally, using numerical modeling, the net and gross potential rates of annual and cumulative sediment transport, as well as shoreline changes after 12 years, were simulated. The effect and length of sedimentation behind the port's breakwater after 1, 5, 10 and 12 years are 81, 190, 247 and 267 meters, respectively, which is in good agreement with the actual observations. Considering the fact that the length of the breakwaters is 300 meters, the sedimentation problem has not yet been established for the port after 12 years.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/44479108" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="dada185238d78376d8d0a29a66a89c65" rel="nofollow" data-download="{"attachment_id":64909702,"asset_id":44479108,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/64909702/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="56761723" href="https://amirkabir.academia.edu/MiladBamdadinejad">Milad Bamdadinejad</a><script data-card-contents-for-user="56761723" type="text/json">{"id":56761723,"first_name":"Milad","last_name":"Bamdadinejad","domain_name":"amirkabir","page_name":"MiladBamdadinejad","display_name":"Milad Bamdadinejad","profile_url":"https://amirkabir.academia.edu/MiladBamdadinejad?f_ri=43335","photo":"https://0.academia-photos.com/56761723/34721215/37297681/s65_milad.bamdadinejad.jpg"}</script></span></span></li><li class="js-paper-rank-work_44479108 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="44479108"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 44479108, container: ".js-paper-rank-work_44479108", }); });</script></li><li class="js-percentile-work_44479108 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 44479108; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_44479108"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_44479108 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="44479108"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 44479108; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=44479108]").text(description); $(".js-view-count-work_44479108").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_44479108").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="44479108"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">3</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="40021" href="https://www.academia.edu/Documents/in/Coastal_Zone_Management">Coastal Zone Management</a>, <script data-card-contents-for-ri="40021" type="text/json">{"id":40021,"name":"Coastal Zone Management","url":"https://www.academia.edu/Documents/in/Coastal_Zone_Management?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="43335" href="https://www.academia.edu/Documents/in/Shoreline_Management_Planning">Shoreline Management Planning</a>, <script data-card-contents-for-ri="43335" type="text/json">{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="82729" href="https://www.academia.edu/Documents/in/Coastal_and_Estuarine_Sediment_Transport">Coastal and Estuarine Sediment Transport</a><script data-card-contents-for-ri="82729" type="text/json">{"id":82729,"name":"Coastal and Estuarine Sediment Transport","url":"https://www.academia.edu/Documents/in/Coastal_and_Estuarine_Sediment_Transport?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=44479108]'), work: {"id":44479108,"title":"Numerical Modeling of Sediment Transport Rate and Shoreline Changes of Jazireh-e Shomali-Jonoubi Port in the Persian Gulf","created_at":"2020-11-11T12:23:18.495-08:00","url":"https://www.academia.edu/44479108/Numerical_Modeling_of_Sediment_Transport_Rate_and_Shoreline_Changes_of_Jazireh_e_Shomali_Jonoubi_Port_in_the_Persian_Gulf?f_ri=43335","dom_id":"work_44479108","summary":"Studying the sediments and predicting the coastal morphological changes have wide applications in coastal engineering, including coastal management, operation, and design of the structures as well as their maintenance, development, and expansion of coasts and coastal structures, which are of paramount importance. The aims of this study are to model the shoreline changes around the Jazireh-e Shomali-Jonoubi Port, calculate the amount of advancement and recession due to the construction of the breakwater, and to determine the areas exposed to erosion and sedimentation. To this end, a series of primary information, including aerial and satellite images, hydrographic and topographic maps, and the specifications and grading of the sediment of the considered coast, has been collected and the overall morphology of the area has been determined. The input data into the model include a 12-year time series of the wave (height, period, and direction of the wave) and the wave climate. The length of the shoreline is 4 km and a profile perpendicular to the coast with a length of 1500 m has been applied to the model. Finally, using numerical modeling, the net and gross potential rates of annual and cumulative sediment transport, as well as shoreline changes after 12 years, were simulated. The effect and length of sedimentation behind the port's breakwater after 1, 5, 10 and 12 years are 81, 190, 247 and 267 meters, respectively, which is in good agreement with the actual observations. Considering the fact that the length of the breakwaters is 300 meters, the sedimentation problem has not yet been established for the port after 12 years.","downloadable_attachments":[{"id":64909702,"asset_id":44479108,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":56761723,"first_name":"Milad","last_name":"Bamdadinejad","domain_name":"amirkabir","page_name":"MiladBamdadinejad","display_name":"Milad Bamdadinejad","profile_url":"https://amirkabir.academia.edu/MiladBamdadinejad?f_ri=43335","photo":"https://0.academia-photos.com/56761723/34721215/37297681/s65_milad.bamdadinejad.jpg"}],"research_interests":[{"id":40021,"name":"Coastal Zone Management","url":"https://www.academia.edu/Documents/in/Coastal_Zone_Management?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false},{"id":82729,"name":"Coastal and Estuarine Sediment Transport","url":"https://www.academia.edu/Documents/in/Coastal_and_Estuarine_Sediment_Transport?f_ri=43335","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_2586625" data-work_id="2586625" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/2586625/Anthony_E_J_2009_Shore_processes_and_their_palaeoenvironmental_applications">Anthony E.J., (2009), Shore processes and their palaeoenvironmental applications</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/2586625" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="b93b3789b6b873d69522528f1c17b78d" rel="nofollow" data-download="{"attachment_id":35460742,"asset_id":2586625,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/35460742/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="514788" href="https://univ-amu.academia.edu/ChristopheMorhange">Christophe Morhange</a><script data-card-contents-for-user="514788" type="text/json">{"id":514788,"first_name":"Christophe","last_name":"Morhange","domain_name":"univ-amu","page_name":"ChristopheMorhange","display_name":"Christophe Morhange","profile_url":"https://univ-amu.academia.edu/ChristopheMorhange?f_ri=43335","photo":"https://0.academia-photos.com/514788/213655/249510/s65_christophe.morhange.jpg"}</script></span></span></li><li class="js-paper-rank-work_2586625 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="2586625"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 2586625, container: ".js-paper-rank-work_2586625", }); 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$(".js-view-count[data-work-id=2586625]").text(description); $(".js-view-count-work_2586625").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_2586625").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="2586625"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">6</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="2637" href="https://www.academia.edu/Documents/in/Coastal_Processes">Coastal Processes</a>, <script data-card-contents-for-ri="2637" type="text/json">{"id":2637,"name":"Coastal Processes","url":"https://www.academia.edu/Documents/in/Coastal_Processes?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="6808" href="https://www.academia.edu/Documents/in/Coastal_Geomorphology">Coastal Geomorphology</a>, <script data-card-contents-for-ri="6808" type="text/json">{"id":6808,"name":"Coastal Geomorphology","url":"https://www.academia.edu/Documents/in/Coastal_Geomorphology?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="7807" href="https://www.academia.edu/Documents/in/Coral_Reefs">Coral Reefs</a>, <script data-card-contents-for-ri="7807" type="text/json">{"id":7807,"name":"Coral Reefs","url":"https://www.academia.edu/Documents/in/Coral_Reefs?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="7808" href="https://www.academia.edu/Documents/in/Mangroves">Mangroves</a><script data-card-contents-for-ri="7808" type="text/json">{"id":7808,"name":"Mangroves","url":"https://www.academia.edu/Documents/in/Mangroves?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=2586625]'), work: {"id":2586625,"title":"Anthony E.J., (2009), Shore processes and their palaeoenvironmental applications","created_at":"2013-02-17T00:11:38.775-08:00","url":"https://www.academia.edu/2586625/Anthony_E_J_2009_Shore_processes_and_their_palaeoenvironmental_applications?f_ri=43335","dom_id":"work_2586625","summary":null,"downloadable_attachments":[{"id":35460742,"asset_id":2586625,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":514788,"first_name":"Christophe","last_name":"Morhange","domain_name":"univ-amu","page_name":"ChristopheMorhange","display_name":"Christophe Morhange","profile_url":"https://univ-amu.academia.edu/ChristopheMorhange?f_ri=43335","photo":"https://0.academia-photos.com/514788/213655/249510/s65_christophe.morhange.jpg"}],"research_interests":[{"id":2637,"name":"Coastal Processes","url":"https://www.academia.edu/Documents/in/Coastal_Processes?f_ri=43335","nofollow":false},{"id":6808,"name":"Coastal Geomorphology","url":"https://www.academia.edu/Documents/in/Coastal_Geomorphology?f_ri=43335","nofollow":false},{"id":7807,"name":"Coral Reefs","url":"https://www.academia.edu/Documents/in/Coral_Reefs?f_ri=43335","nofollow":false},{"id":7808,"name":"Mangroves","url":"https://www.academia.edu/Documents/in/Mangroves?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335"},{"id":43390,"name":"Sandy Beaches","url":"https://www.academia.edu/Documents/in/Sandy_Beaches?f_ri=43335"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_49064875" data-work_id="49064875" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/49064875/Dorchester_County_Maryland_Heritage_Area_Lecture_5_27_2021_SEA_LEVEL_RISE_AND_COASTAL_EROSION_SUMMARY">Dorchester County Maryland Heritage Area Lecture 5-27-2021 SEA LEVEL RISE AND COASTAL EROSION SUMMARY</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">As an invited speaker, the following presentation was given to the Heritage Area Board members on May 27th, 2021. The presentation biriefly summarizes my investigation into recent sea level rise and coastal erosion issues in Dorchester... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_49064875" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">As an invited speaker, the following presentation was given to the Heritage Area Board members on May 27th, 2021.  The presentation biriefly summarizes my investigation into recent sea level rise and coastal erosion issues in Dorchester County.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/49064875" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="adc92a3cca4395be26a0d27972b63200" rel="nofollow" data-download="{"attachment_id":67456432,"asset_id":49064875,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/67456432/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="2817549" href="https://si.academia.edu/DarrinLowery">Darrin Lowery</a><script data-card-contents-for-user="2817549" type="text/json">{"id":2817549,"first_name":"Darrin","last_name":"Lowery","domain_name":"si","page_name":"DarrinLowery","display_name":"Darrin Lowery","profile_url":"https://si.academia.edu/DarrinLowery?f_ri=43335","photo":"https://0.academia-photos.com/2817549/990298/15490945/s65_darrin.lowery.jpg"}</script></span></span></li><li class="js-paper-rank-work_49064875 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="49064875"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 49064875, container: ".js-paper-rank-work_49064875", }); 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$(".js-view-count[data-work-id=49064875]").text(description); $(".js-view-count-work_49064875").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_49064875").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="49064875"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">16</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="399" href="https://www.academia.edu/Documents/in/Prehistoric_Archaeology">Prehistoric Archaeology</a>, <script data-card-contents-for-ri="399" type="text/json">{"id":399,"name":"Prehistoric Archaeology","url":"https://www.academia.edu/Documents/in/Prehistoric_Archaeology?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="1275" href="https://www.academia.edu/Documents/in/Coastal_Management">Coastal Management</a>, <script data-card-contents-for-ri="1275" type="text/json">{"id":1275,"name":"Coastal Management","url":"https://www.academia.edu/Documents/in/Coastal_Management?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="5053" href="https://www.academia.edu/Documents/in/North_American_Archaeology_">North American (Archaeology)</a>, <script data-card-contents-for-ri="5053" type="text/json">{"id":5053,"name":"North American (Archaeology)","url":"https://www.academia.edu/Documents/in/North_American_Archaeology_?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="5054" href="https://www.academia.edu/Documents/in/Northeastern_North_America_Archaeology_">Northeastern North America (Archaeology)</a><script data-card-contents-for-ri="5054" type="text/json">{"id":5054,"name":"Northeastern North America (Archaeology)","url":"https://www.academia.edu/Documents/in/Northeastern_North_America_Archaeology_?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=49064875]'), work: {"id":49064875,"title":"Dorchester County Maryland Heritage Area Lecture 5-27-2021 SEA LEVEL RISE AND COASTAL EROSION SUMMARY","created_at":"2021-05-29T03:37:49.564-07:00","url":"https://www.academia.edu/49064875/Dorchester_County_Maryland_Heritage_Area_Lecture_5_27_2021_SEA_LEVEL_RISE_AND_COASTAL_EROSION_SUMMARY?f_ri=43335","dom_id":"work_49064875","summary":"As an invited speaker, the following presentation was given to the Heritage Area Board members on May 27th, 2021. The presentation biriefly summarizes my investigation into recent sea level rise and coastal erosion issues in Dorchester County. ","downloadable_attachments":[{"id":67456432,"asset_id":49064875,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":2817549,"first_name":"Darrin","last_name":"Lowery","domain_name":"si","page_name":"DarrinLowery","display_name":"Darrin Lowery","profile_url":"https://si.academia.edu/DarrinLowery?f_ri=43335","photo":"https://0.academia-photos.com/2817549/990298/15490945/s65_darrin.lowery.jpg"}],"research_interests":[{"id":399,"name":"Prehistoric Archaeology","url":"https://www.academia.edu/Documents/in/Prehistoric_Archaeology?f_ri=43335","nofollow":false},{"id":1275,"name":"Coastal Management","url":"https://www.academia.edu/Documents/in/Coastal_Management?f_ri=43335","nofollow":false},{"id":5053,"name":"North American (Archaeology)","url":"https://www.academia.edu/Documents/in/North_American_Archaeology_?f_ri=43335","nofollow":false},{"id":5054,"name":"Northeastern North America (Archaeology)","url":"https://www.academia.edu/Documents/in/Northeastern_North_America_Archaeology_?f_ri=43335","nofollow":false},{"id":14492,"name":"Coastal and Island Archaeology","url":"https://www.academia.edu/Documents/in/Coastal_and_Island_Archaeology?f_ri=43335"},{"id":18625,"name":"Sea Level","url":"https://www.academia.edu/Documents/in/Sea_Level?f_ri=43335"},{"id":18935,"name":"Impact of climate change on sea level rise","url":"https://www.academia.edu/Documents/in/Impact_of_climate_change_on_sea_level_rise?f_ri=43335"},{"id":27086,"name":"Coastal Erosion","url":"https://www.academia.edu/Documents/in/Coastal_Erosion?f_ri=43335"},{"id":30368,"name":"Chesapeake Colonial History","url":"https://www.academia.edu/Documents/in/Chesapeake_Colonial_History?f_ri=43335"},{"id":32163,"name":"Holocene sea level change","url":"https://www.academia.edu/Documents/in/Holocene_sea_level_change?f_ri=43335"},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335"},{"id":72498,"name":"Sea level rise","url":"https://www.academia.edu/Documents/in/Sea_level_rise?f_ri=43335"},{"id":129829,"name":"Archaeology of Southeastern United States","url":"https://www.academia.edu/Documents/in/Archaeology_of_Southeastern_United_States?f_ri=43335"},{"id":224646,"name":"Shoreline Dynamics","url":"https://www.academia.edu/Documents/in/Shoreline_Dynamics?f_ri=43335"},{"id":246329,"name":"Environmental/coastal erosion/Sea Level Rise","url":"https://www.academia.edu/Documents/in/Environmental_coastal_erosion_Sea_Level_Rise?f_ri=43335"},{"id":714505,"name":"Shoreline Studies","url":"https://www.academia.edu/Documents/in/Shoreline_Studies?f_ri=43335"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_1079559" data-work_id="1079559" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/1079559/Shoreline_urbanization_reduces_terrestrial_insect_subsidies_to_fishes_in_North_American_lakes">Shoreline urbanization reduces terrestrial insect subsidies to fishes in North American lakes</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/1079559" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="decef537498a24cb5433de1c1132e2d4" rel="nofollow" data-download="{"attachment_id":6611507,"asset_id":1079559,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/6611507/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="930408" href="https://tacoma-washington.academia.edu/TessaFrancis">Tessa Francis</a><script data-card-contents-for-user="930408" type="text/json">{"id":930408,"first_name":"Tessa","last_name":"Francis","domain_name":"tacoma-washington","page_name":"TessaFrancis","display_name":"Tessa Francis","profile_url":"https://tacoma-washington.academia.edu/TessaFrancis?f_ri=43335","photo":"https://0.academia-photos.com/930408/434513/11792874/s65_tessa.francis.jpg"}</script></span></span></li><li class="js-paper-rank-work_1079559 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="1079559"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 1079559, container: ".js-paper-rank-work_1079559", }); });</script></li><li class="js-percentile-work_1079559 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x 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Ecology","url":"https://www.academia.edu/Documents/in/Fish_Ecology?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="24646" href="https://www.academia.edu/Documents/in/Food_web_ecology">Food web ecology</a>, <script data-card-contents-for-ri="24646" type="text/json">{"id":24646,"name":"Food web ecology","url":"https://www.academia.edu/Documents/in/Food_web_ecology?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="27190" href="https://www.academia.edu/Documents/in/Insect_Ecology">Insect Ecology</a><script data-card-contents-for-ri="27190" type="text/json">{"id":27190,"name":"Insect Ecology","url":"https://www.academia.edu/Documents/in/Insect_Ecology?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=1079559]'), work: {"id":1079559,"title":"Shoreline urbanization reduces terrestrial insect subsidies to fishes in North American lakes","created_at":"2011-11-10T03:28:52.260-08:00","url":"https://www.academia.edu/1079559/Shoreline_urbanization_reduces_terrestrial_insect_subsidies_to_fishes_in_North_American_lakes?f_ri=43335","dom_id":"work_1079559","summary":null,"downloadable_attachments":[{"id":6611507,"asset_id":1079559,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":930408,"first_name":"Tessa","last_name":"Francis","domain_name":"tacoma-washington","page_name":"TessaFrancis","display_name":"Tessa Francis","profile_url":"https://tacoma-washington.academia.edu/TessaFrancis?f_ri=43335","photo":"https://0.academia-photos.com/930408/434513/11792874/s65_tessa.francis.jpg"}],"research_interests":[{"id":1999,"name":"Limnology","url":"https://www.academia.edu/Documents/in/Limnology?f_ri=43335","nofollow":false},{"id":22435,"name":"Fish Ecology","url":"https://www.academia.edu/Documents/in/Fish_Ecology?f_ri=43335","nofollow":false},{"id":24646,"name":"Food web ecology","url":"https://www.academia.edu/Documents/in/Food_web_ecology?f_ri=43335","nofollow":false},{"id":27190,"name":"Insect Ecology","url":"https://www.academia.edu/Documents/in/Insect_Ecology?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335"},{"id":224646,"name":"Shoreline Dynamics","url":"https://www.academia.edu/Documents/in/Shoreline_Dynamics?f_ri=43335"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_42641811" data-work_id="42641811" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/42641811/Short_time_analysis_of_shoreline_based_on_RapidEye_satellite_images_in_the_terminal_area_of_Pec%C3%A9m_Port_Cear%C3%A1_Brazil">Short-time analysis of shoreline based on RapidEye satellite images in the terminal area of Pecém Port, Ceará, Brazil</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Coastal environments are highly dynamic and sensitive to interference and variations caused by the numerous natural and anthropogenic agents. The northern coast of Northeastern Brazil has undergone intense erosion in recent years.... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_42641811" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Coastal environments are highly dynamic and sensitive to interference and variations caused by the numerous natural and anthropogenic agents. The northern coast of Northeastern Brazil has undergone intense erosion in recent years. However, the construction of the Pecém Port modified the beach and shoreline features differently from the adjacent areas. This article describes using remote-sensing images integrated with a Geographic Information System to evaluate the sedimentary balance and morphological changes observed in the sandy beach area that was affected by the construction of Pecém Port. Two methods were applied to the RapidEye images to quantify the short-time changes that occurred on the coast. The Digital Shoreline Analysis System method showed that the beach width increased west to the port, which was calculated by the Change Polygon Approach determined by intersecting and uniting polygons to estimate the difference between the areas over time. The short-time analysis results showed changing coastal morphology, demonstrating that the anthropic interventions in the region are transforming significantly the natural elements that make up the region landscape. Between 2011 and 2014, the investigated beach stretch of approximately 3 km suffered an accretion process of more than 102,000 m2 over 3 years. The high spatial resolution of satellite images, digital processing imaging techniques and geostatistical methods were effective in this study, allowing understanding the recent changes in the area.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/42641811" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="34bf7201dbf87a5429f7577f92afe005" rel="nofollow" data-download="{"attachment_id":62847564,"asset_id":42641811,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/62847564/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="30091165" href="https://independent.academia.edu/claudioangeloneto">Cláudio Ângelo da Silva Neto</a><script data-card-contents-for-user="30091165" type="text/json">{"id":30091165,"first_name":"Cláudio Ângelo","last_name":"da Silva Neto","domain_name":"independent","page_name":"claudioangeloneto","display_name":"Cláudio Ângelo da Silva Neto","profile_url":"https://independent.academia.edu/claudioangeloneto?f_ri=43335","photo":"https://0.academia-photos.com/30091165/8692184/29458137/s65_cl_udio_ngelo.da_silva_neto.jpg"}</script></span></span></li><li class="js-paper-rank-work_42641811 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="42641811"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 42641811, container: ".js-paper-rank-work_42641811", }); 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$(".js-view-count[data-work-id=42641811]").text(description); $(".js-view-count-work_42641811").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_42641811").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="42641811"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">13</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="1275" href="https://www.academia.edu/Documents/in/Coastal_Management">Coastal Management</a>, <script data-card-contents-for-ri="1275" type="text/json">{"id":1275,"name":"Coastal Management","url":"https://www.academia.edu/Documents/in/Coastal_Management?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="1286" href="https://www.academia.edu/Documents/in/Coastal_Engineering">Coastal Engineering</a>, <script data-card-contents-for-ri="1286" type="text/json">{"id":1286,"name":"Coastal Engineering","url":"https://www.academia.edu/Documents/in/Coastal_Engineering?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="2637" href="https://www.academia.edu/Documents/in/Coastal_Processes">Coastal Processes</a>, <script data-card-contents-for-ri="2637" type="text/json">{"id":2637,"name":"Coastal Processes","url":"https://www.academia.edu/Documents/in/Coastal_Processes?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="6808" href="https://www.academia.edu/Documents/in/Coastal_Geomorphology">Coastal Geomorphology</a><script data-card-contents-for-ri="6808" type="text/json">{"id":6808,"name":"Coastal Geomorphology","url":"https://www.academia.edu/Documents/in/Coastal_Geomorphology?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=42641811]'), work: {"id":42641811,"title":"Short-time analysis of shoreline based on RapidEye satellite images in the terminal area of Pecém Port, Ceará, Brazil","created_at":"2020-04-06T08:16:54.871-07:00","url":"https://www.academia.edu/42641811/Short_time_analysis_of_shoreline_based_on_RapidEye_satellite_images_in_the_terminal_area_of_Pec%C3%A9m_Port_Cear%C3%A1_Brazil?f_ri=43335","dom_id":"work_42641811","summary":"Coastal environments are highly dynamic and sensitive to interference and variations caused by the numerous natural and anthropogenic agents. The northern coast of Northeastern Brazil has undergone intense erosion in recent years. However, the construction of the Pecém Port modified the beach and shoreline features differently from the adjacent areas. This article describes using remote-sensing images integrated with a Geographic Information System to evaluate the sedimentary balance and morphological changes observed in the sandy beach area that was affected by the construction of Pecém Port. Two methods were applied to the RapidEye images to quantify the short-time changes that occurred on the coast. The Digital Shoreline Analysis System method showed that the beach width increased west to the port, which was calculated by the Change Polygon Approach determined by intersecting and uniting polygons to estimate the difference between the areas over time. The short-time analysis results showed changing coastal morphology, demonstrating that the anthropic interventions in the region are transforming significantly the natural elements that make up the region landscape. Between 2011 and 2014, the investigated beach stretch of approximately 3 km suffered an accretion process of more than 102,000 m2 over 3 years. The high spatial resolution of satellite images, digital processing imaging techniques and geostatistical methods were effective in this study, allowing understanding the recent changes in the area.","downloadable_attachments":[{"id":62847564,"asset_id":42641811,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":30091165,"first_name":"Cláudio Ângelo","last_name":"da Silva Neto","domain_name":"independent","page_name":"claudioangeloneto","display_name":"Cláudio Ângelo da Silva Neto","profile_url":"https://independent.academia.edu/claudioangeloneto?f_ri=43335","photo":"https://0.academia-photos.com/30091165/8692184/29458137/s65_cl_udio_ngelo.da_silva_neto.jpg"}],"research_interests":[{"id":1275,"name":"Coastal Management","url":"https://www.academia.edu/Documents/in/Coastal_Management?f_ri=43335","nofollow":false},{"id":1286,"name":"Coastal Engineering","url":"https://www.academia.edu/Documents/in/Coastal_Engineering?f_ri=43335","nofollow":false},{"id":2637,"name":"Coastal Processes","url":"https://www.academia.edu/Documents/in/Coastal_Processes?f_ri=43335","nofollow":false},{"id":6808,"name":"Coastal Geomorphology","url":"https://www.academia.edu/Documents/in/Coastal_Geomorphology?f_ri=43335","nofollow":false},{"id":27086,"name":"Coastal Erosion","url":"https://www.academia.edu/Documents/in/Coastal_Erosion?f_ri=43335"},{"id":40021,"name":"Coastal Zone Management","url":"https://www.academia.edu/Documents/in/Coastal_Zone_Management?f_ri=43335"},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335"},{"id":170868,"name":"Climate impacts on shorelines and dunes","url":"https://www.academia.edu/Documents/in/Climate_impacts_on_shorelines_and_dunes?f_ri=43335"},{"id":440716,"name":"Remote Sensing for Shoreline Change","url":"https://www.academia.edu/Documents/in/Remote_Sensing_for_Shoreline_Change?f_ri=43335"},{"id":515102,"name":"Shorelines","url":"https://www.academia.edu/Documents/in/Shorelines?f_ri=43335"},{"id":714505,"name":"Shoreline Studies","url":"https://www.academia.edu/Documents/in/Shoreline_Studies?f_ri=43335"},{"id":958692,"name":"Coastline","url":"https://www.academia.edu/Documents/in/Coastline?f_ri=43335"},{"id":1210027,"name":"Shoreline Changes","url":"https://www.academia.edu/Documents/in/Shoreline_Changes?f_ri=43335"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_40691175" data-work_id="40691175" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/40691175/Coastlines_and_Communities_A_Preliminary_Glance_at_the_Relationship_between_Shoreline_Armoring_and_Sense_of_Place_in_Puget_Sound">Coastlines and Communities: A Preliminary Glance at the Relationship between Shoreline Armoring and Sense of Place in Puget Sound</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/40691175" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="6115edfd40d44c8c9c70f5dcc1d06848" rel="nofollow" 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type="text/json">{"id":1387432,"first_name":"David","last_name":"Trimbach","domain_name":"washingtondepartmentfishwildlife","page_name":"DavidTrimbach","display_name":"David J Trimbach","profile_url":"https://washingtondepartmentfishwildlife.academia.edu/DavidTrimbach?f_ri=43335","photo":"https://0.academia-photos.com/1387432/604730/38471880/s65_david.trimbach.jpg"}</script></span></span></li><li class="js-paper-rank-work_40691175 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="40691175"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 40691175, container: ".js-paper-rank-work_40691175", }); });</script></li><li class="js-percentile-work_40691175 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: 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Geography</a>, <script data-card-contents-for-ri="263" type="text/json">{"id":263,"name":"Cultural Geography","url":"https://www.academia.edu/Documents/in/Cultural_Geography?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="1275" href="https://www.academia.edu/Documents/in/Coastal_Management">Coastal Management</a>, <script data-card-contents-for-ri="1275" type="text/json">{"id":1275,"name":"Coastal Management","url":"https://www.academia.edu/Documents/in/Coastal_Management?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="2319" href="https://www.academia.edu/Documents/in/Place_Attachment">Place Attachment</a><script data-card-contents-for-ri="2319" type="text/json">{"id":2319,"name":"Place Attachment","url":"https://www.academia.edu/Documents/in/Place_Attachment?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=40691175]'), work: {"id":40691175,"title":"Coastlines and Communities: A Preliminary Glance at the Relationship between Shoreline Armoring and Sense of Place in Puget Sound","created_at":"2019-10-21T14:57:06.476-07:00","url":"https://www.academia.edu/40691175/Coastlines_and_Communities_A_Preliminary_Glance_at_the_Relationship_between_Shoreline_Armoring_and_Sense_of_Place_in_Puget_Sound?f_ri=43335","dom_id":"work_40691175","summary":null,"downloadable_attachments":[{"id":60974847,"asset_id":40691175,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":1387432,"first_name":"David","last_name":"Trimbach","domain_name":"washingtondepartmentfishwildlife","page_name":"DavidTrimbach","display_name":"David J Trimbach","profile_url":"https://washingtondepartmentfishwildlife.academia.edu/DavidTrimbach?f_ri=43335","photo":"https://0.academia-photos.com/1387432/604730/38471880/s65_david.trimbach.jpg"}],"research_interests":[{"id":262,"name":"Human Geography","url":"https://www.academia.edu/Documents/in/Human_Geography?f_ri=43335","nofollow":false},{"id":263,"name":"Cultural Geography","url":"https://www.academia.edu/Documents/in/Cultural_Geography?f_ri=43335","nofollow":false},{"id":1275,"name":"Coastal Management","url":"https://www.academia.edu/Documents/in/Coastal_Management?f_ri=43335","nofollow":false},{"id":2319,"name":"Place Attachment","url":"https://www.academia.edu/Documents/in/Place_Attachment?f_ri=43335","nofollow":false},{"id":2433,"name":"Place and Identity","url":"https://www.academia.edu/Documents/in/Place_and_Identity?f_ri=43335"},{"id":6807,"name":"Coastal Geography","url":"https://www.academia.edu/Documents/in/Coastal_Geography?f_ri=43335"},{"id":7624,"name":"Place Identity","url":"https://www.academia.edu/Documents/in/Place_Identity?f_ri=43335"},{"id":12200,"name":"Sense of Place","url":"https://www.academia.edu/Documents/in/Sense_of_Place?f_ri=43335"},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335"},{"id":714505,"name":"Shoreline Studies","url":"https://www.academia.edu/Documents/in/Shoreline_Studies?f_ri=43335"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_261175" data-work_id="261175" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/261175/_The_environmental_effects_of_wave_energy_converter_arrays_upon_the_intertidal_zone_YCSEC09_Poster">"The environmental effects of wave energy converter arrays upon the intertidal zone." YCSEC'09 Poster</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The environmental effect of the reduction of wave energy impacting upon the coastline is one that is not well understood, not just because of the highly dynamic environment, but also due to the difficulty and cost of measuring a... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_261175" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The environmental effect of the reduction of wave energy impacting upon the coastline is one that is not well understood, not just because of the highly dynamic environment, but also due to the difficulty and cost of measuring a quantitative value of the wave energy regime. There are many variables which ultimately determine the wave action on a particular point on the shoreline and many more which directly affect the organisms in that environment; wave action is just one of 44 main variables that need to be taken into consideration.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/261175" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="9b1a9361cbdfa3ac0214ab156c845044" rel="nofollow" data-download="{"attachment_id":1094160,"asset_id":261175,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/1094160/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="6524" href="https://hw.academia.edu/RobertBeharie">Robert A Beharie</a><script data-card-contents-for-user="6524" type="text/json">{"id":6524,"first_name":"Robert","last_name":"Beharie","domain_name":"hw","page_name":"RobertBeharie","display_name":"Robert A Beharie","profile_url":"https://hw.academia.edu/RobertBeharie?f_ri=43335","photo":"https://0.academia-photos.com/6524/2515/120353/s65_robert.beharie.jpg"}</script></span></span></li><li class="js-paper-rank-work_261175 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="261175"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 261175, container: ".js-paper-rank-work_261175", }); });</script></li><li class="js-percentile-work_261175 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 261175; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_261175"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_261175 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="261175"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 261175; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=261175]").text(description); $(".js-view-count-work_261175").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_261175").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="261175"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">4</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="2800" href="https://www.academia.edu/Documents/in/Marine_Renewable_Energy">Marine Renewable Energy</a>, <script data-card-contents-for-ri="2800" type="text/json">{"id":2800,"name":"Marine Renewable Energy","url":"https://www.academia.edu/Documents/in/Marine_Renewable_Energy?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="4035" href="https://www.academia.edu/Documents/in/Marine_Ecology">Marine Ecology</a>, <script data-card-contents-for-ri="4035" type="text/json">{"id":4035,"name":"Marine Ecology","url":"https://www.academia.edu/Documents/in/Marine_Ecology?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="16441" href="https://www.academia.edu/Documents/in/Marine_Science">Marine Science</a>, <script data-card-contents-for-ri="16441" type="text/json">{"id":16441,"name":"Marine Science","url":"https://www.academia.edu/Documents/in/Marine_Science?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="43335" href="https://www.academia.edu/Documents/in/Shoreline_Management_Planning">Shoreline Management Planning</a><script data-card-contents-for-ri="43335" type="text/json">{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=261175]'), work: {"id":261175,"title":"\"The environmental effects of wave energy converter arrays upon the intertidal zone.\" YCSEC'09 Poster","created_at":"2010-07-11T22:32:31.563-07:00","url":"https://www.academia.edu/261175/_The_environmental_effects_of_wave_energy_converter_arrays_upon_the_intertidal_zone_YCSEC09_Poster?f_ri=43335","dom_id":"work_261175","summary":"The environmental effect of the reduction of wave energy impacting upon the coastline is one that is not well understood, not just because of the highly dynamic environment, but also due to the difficulty and cost of measuring a quantitative value of the wave energy regime. There are many variables which ultimately determine the wave action on a particular point on the shoreline and many more which directly affect the organisms in that environment; wave action is just one of 44 main variables that need to be taken into consideration.","downloadable_attachments":[{"id":1094160,"asset_id":261175,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":6524,"first_name":"Robert","last_name":"Beharie","domain_name":"hw","page_name":"RobertBeharie","display_name":"Robert A Beharie","profile_url":"https://hw.academia.edu/RobertBeharie?f_ri=43335","photo":"https://0.academia-photos.com/6524/2515/120353/s65_robert.beharie.jpg"}],"research_interests":[{"id":2800,"name":"Marine Renewable Energy","url":"https://www.academia.edu/Documents/in/Marine_Renewable_Energy?f_ri=43335","nofollow":false},{"id":4035,"name":"Marine Ecology","url":"https://www.academia.edu/Documents/in/Marine_Ecology?f_ri=43335","nofollow":false},{"id":16441,"name":"Marine Science","url":"https://www.academia.edu/Documents/in/Marine_Science?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_16956292" data-work_id="16956292" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/16956292/Shoreline_Management_Planning_Can_It_Benefit_Ghana_A_Case_Study_of_UK_SMPs_and_Their_Potential_Relevance_in_Ghana">Shoreline Management Planning: Can It Benefit Ghana? A Case Study of UK SMPs and Their Potential Relevance in Ghana</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">This paper assesses the potential for the adaptation of UK Shoreline Management Planning to address Ghana’s problems of coastal erosion and resultant shoreline retreat in an environmentally acceptable and sustainable way. Management... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_16956292" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">This paper assesses the potential for the adaptation of UK Shoreline Management Planning to address Ghana’s problems of coastal erosion and resultant shoreline retreat in an environmentally acceptable and sustainable way. Management strategies, past and existing, have largely focussed upon provision of hard protection at specific locations where risk levels to life and economic assets are high. There has been little commitment to the concepts of integration of management interventions with wider natural processes and longer-term sustainability. In most cases, such ‘ad hoc’ management interventions classically tend to stabilise the shoreline at the protected section and aggravate the situation elsewhere along the shoreline (“knock-on effects”).  <br />Such problems have occurred previously on many other developed coastlines leading in recent decades to more holistic and potentially sustainable shoreline management methods (Hooke, 1999). For example, UK shoreline management planning since the mid 1990s has achieved success in reducing the occurrence of “knock on effects.” It has altered thinking away from the basic provision of defences towards a more holistic management of risks at the coast, setting out clearly locations where protection is likely to be required and others where alternative options are more sustainable. This paper reviews the progress achieved in the UK and assesses the extent to which the methods devised could be adapted towards the requirements of Ghana’s shoreline. It concludes that many of the concepts and methods should be transferable provided that a sound understanding is developed of the physical coastal processes based on application of littoral cell and sediment budget methodology.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/16956292" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="c389496a2b80aed8f3841dbe1d812ee9" rel="nofollow" data-download="{"attachment_id":39276461,"asset_id":16956292,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/39276461/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="36417750" href="https://port.academia.edu/IsaacBoateng">Isaac Boateng</a><script data-card-contents-for-user="36417750" type="text/json">{"id":36417750,"first_name":"Isaac","last_name":"Boateng","domain_name":"port","page_name":"IsaacBoateng","display_name":"Isaac Boateng","profile_url":"https://port.academia.edu/IsaacBoateng?f_ri=43335","photo":"https://0.academia-photos.com/36417750/10467533/11679797/s65_isaac.boateng.png"}</script></span></span></li><li class="js-paper-rank-work_16956292 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="16956292"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 16956292, container: ".js-paper-rank-work_16956292", }); 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$(".js-view-count[data-work-id=16956292]").text(description); $(".js-view-count-work_16956292").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_16956292").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="16956292"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">3</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="1275" href="https://www.academia.edu/Documents/in/Coastal_Management">Coastal Management</a>, <script data-card-contents-for-ri="1275" type="text/json">{"id":1275,"name":"Coastal Management","url":"https://www.academia.edu/Documents/in/Coastal_Management?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="2637" href="https://www.academia.edu/Documents/in/Coastal_Processes">Coastal Processes</a>, <script data-card-contents-for-ri="2637" type="text/json">{"id":2637,"name":"Coastal Processes","url":"https://www.academia.edu/Documents/in/Coastal_Processes?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="43335" href="https://www.academia.edu/Documents/in/Shoreline_Management_Planning">Shoreline Management Planning</a><script data-card-contents-for-ri="43335" type="text/json">{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=16956292]'), work: {"id":16956292,"title":"Shoreline Management Planning: Can It Benefit Ghana? A Case Study of UK SMPs and Their Potential Relevance in Ghana","created_at":"2015-10-18T10:10:57.897-07:00","url":"https://www.academia.edu/16956292/Shoreline_Management_Planning_Can_It_Benefit_Ghana_A_Case_Study_of_UK_SMPs_and_Their_Potential_Relevance_in_Ghana?f_ri=43335","dom_id":"work_16956292","summary":"This paper assesses the potential for the adaptation of UK Shoreline Management Planning to address Ghana’s problems of coastal erosion and resultant shoreline retreat in an environmentally acceptable and sustainable way. Management strategies, past and existing, have largely focussed upon provision of hard protection at specific locations where risk levels to life and economic assets are high. There has been little commitment to the concepts of integration of management interventions with wider natural processes and longer-term sustainability. In most cases, such ‘ad hoc’ management interventions classically tend to stabilise the shoreline at the protected section and aggravate the situation elsewhere along the shoreline (“knock-on effects”). \nSuch problems have occurred previously on many other developed coastlines leading in recent decades to more holistic and potentially sustainable shoreline management methods (Hooke, 1999). For example, UK shoreline management planning since the mid 1990s has achieved success in reducing the occurrence of “knock on effects.” It has altered thinking away from the basic provision of defences towards a more holistic management of risks at the coast, setting out clearly locations where protection is likely to be required and others where alternative options are more sustainable. This paper reviews the progress achieved in the UK and assesses the extent to which the methods devised could be adapted towards the requirements of Ghana’s shoreline. It concludes that many of the concepts and methods should be transferable provided that a sound understanding is developed of the physical coastal processes based on application of littoral cell and sediment budget methodology. ","downloadable_attachments":[{"id":39276461,"asset_id":16956292,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":36417750,"first_name":"Isaac","last_name":"Boateng","domain_name":"port","page_name":"IsaacBoateng","display_name":"Isaac Boateng","profile_url":"https://port.academia.edu/IsaacBoateng?f_ri=43335","photo":"https://0.academia-photos.com/36417750/10467533/11679797/s65_isaac.boateng.png"}],"research_interests":[{"id":1275,"name":"Coastal Management","url":"https://www.academia.edu/Documents/in/Coastal_Management?f_ri=43335","nofollow":false},{"id":2637,"name":"Coastal Processes","url":"https://www.academia.edu/Documents/in/Coastal_Processes?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_77184692 coauthored" data-work_id="77184692" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/77184692/Using_Arts_based_Education_and_High_School_Students_and_Educators_to_Document_the_Adams_Bay_Mound_Site_Plaquemines_Parish_Louisiana_Gulf_Communities_Research_Institute">Using Arts-based Education and High-School Students and Educators to Document the Adams Bay Mound Site, Plaquemines Parish, Louisiana, Gulf Communities Research Institute</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">In the summer of 2018, the Gulf Communities Research Institute (GCRI) initiated a program of conservation research directed at an archaeological site, the Adams Bay Mounds, located in southern Plaquemines Parish, Louisiana. The Native... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_77184692" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">In the summer of 2018, the Gulf Communities Research Institute (GCRI) initiated a program of conservation research directed at an archaeological site, the Adams Bay Mounds, located in southern Plaquemines Parish, Louisiana. The Native American monumental site was built approximately 600-800 years ago by indigenous peoples who are the ancestors of modern, coastal communities. Conservation research was directed at the site because it has been severely impacted by erosion, changes in environmental chemistry, and sea-level rise over the past 10 years. In this short period of time, archaeologists have observed the last earthen and shell mound at this site slowly erode into the Gulf of Mexico (less than 50% of the mound currently remains). Research at Adams Bay was directed towards documenting the site and teaching young people field science and Native American history through hands-on field experience. Data gathered from fieldwork was used to develop criteria for assessing erosion protection measures at similarly-threatened archaeological sites. Funds from National Geographic were used to measure, draw, document, and otherwise study the earthen mound and to teach high-school students from the New Orleans Center for the Creative Arts about environmental science and archaeology. Students assisted in fieldwork, learned field methods, and generated media (film, photography, mixed-media) based on their experiences.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/77184692" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="9fb159b5492ab3970d7800c01f4d47ec" rel="nofollow" data-download="{"attachment_id":84621363,"asset_id":77184692,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/84621363/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="7129645" href="https://uwyo.academia.edu/BrianOstahowski">Brian Ostahowski</a><script data-card-contents-for-user="7129645" type="text/json">{"id":7129645,"first_name":"Brian","last_name":"Ostahowski","domain_name":"uwyo","page_name":"BrianOstahowski","display_name":"Brian Ostahowski","profile_url":"https://uwyo.academia.edu/BrianOstahowski?f_ri=43335","photo":"https://0.academia-photos.com/7129645/3936043/12593878/s65_brian.ostahowski.jpg"}</script></span></span><span class="u-displayInlineBlock InlineList-item-text"> and <span class="u-textDecorationUnderline u-clickable InlineList-item-text js-work-more-authors-77184692">+1</span><div class="hidden js-additional-users-77184692"><div><span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a href="https://fsu.academia.edu/JayurMehta">Jayur Mehta</a></span></div></div></span><script>(function(){ var popoverSettings = { el: $('.js-work-more-authors-77184692'), placement: 'bottom', hide_delay: 200, html: true, content: function(){ return $('.js-additional-users-77184692').html(); 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The Native American monumental site was built approximately 600-800 years ago by indigenous peoples who are the ancestors of modern, coastal communities. Conservation research was directed at the site because it has been severely impacted by erosion, changes in environmental chemistry, and sea-level rise over the past 10 years. In this short period of time, archaeologists have observed the last earthen and shell mound at this site slowly erode into the Gulf of Mexico (less than 50% of the mound currently remains). Research at Adams Bay was directed towards documenting the site and teaching young people field science and Native American history through hands-on field experience. Data gathered from fieldwork was used to develop criteria for assessing erosion protection measures at similarly-threatened archaeological sites. Funds from National Geographic were used to measure, draw, document, and otherwise study the earthen mound and to teach high-school students from the New Orleans Center for the Creative Arts about environmental science and archaeology. Students assisted in fieldwork, learned field methods, and generated media (film, photography, mixed-media) based on their experiences.","downloadable_attachments":[{"id":84621363,"asset_id":77184692,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":7129645,"first_name":"Brian","last_name":"Ostahowski","domain_name":"uwyo","page_name":"BrianOstahowski","display_name":"Brian Ostahowski","profile_url":"https://uwyo.academia.edu/BrianOstahowski?f_ri=43335","photo":"https://0.academia-photos.com/7129645/3936043/12593878/s65_brian.ostahowski.jpg"},{"id":389661,"first_name":"Jayur","last_name":"Mehta","domain_name":"fsu","page_name":"JayurMehta","display_name":"Jayur Mehta","profile_url":"https://fsu.academia.edu/JayurMehta?f_ri=43335","photo":"https://0.academia-photos.com/389661/2506443/19575936/s65_jayur.mehta.jpg"}],"research_interests":[{"id":14492,"name":"Coastal and Island Archaeology","url":"https://www.academia.edu/Documents/in/Coastal_and_Island_Archaeology?f_ri=43335","nofollow":false},{"id":18088,"name":"Southeastern Archaeology (Archaeology in North America)","url":"https://www.academia.edu/Documents/in/Southeastern_Archaeology_Archaeology_in_North_America_?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false},{"id":49677,"name":"Arts-Based Educational Research","url":"https://www.academia.edu/Documents/in/Arts-Based_Educational_Research?f_ri=43335","nofollow":false},{"id":126506,"name":"Sea-Level Rise","url":"https://www.academia.edu/Documents/in/Sea-Level_Rise?f_ri=43335"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_47243402" data-work_id="47243402" itemscope="itemscope" 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href="https://www.academia.edu/32863631/Erosion_and_Archaeological_Site_Loss_Adjacent_to_the_Chesapeake_Bay_and_the_Atlantic_Coast_pdf">Erosion and Archaeological Site Loss Adjacent to the Chesapeake Bay and the Atlantic Coast.pdf</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest">The brief summary appeared in the 2017 Maryland Archaeology Month booklet.  The summary presents an overview of archaeological site loss due to erosion along the margins of the Chesapeake Bay and Atlantic sea coast.</div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/32863631" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" 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Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335"},{"id":72498,"name":"Sea level rise","url":"https://www.academia.edu/Documents/in/Sea_level_rise?f_ri=43335"},{"id":149686,"name":"Wave and Storm Surge Modelling","url":"https://www.academia.edu/Documents/in/Wave_and_Storm_Surge_Modelling?f_ri=43335"},{"id":352631,"name":"Coastal Flood Hazards","url":"https://www.academia.edu/Documents/in/Coastal_Flood_Hazards?f_ri=43335"},{"id":376098,"name":"El Nino-Southern Oscillation","url":"https://www.academia.edu/Documents/in/El_Nino-Southern_Oscillation?f_ri=43335"},{"id":1150373,"name":"Pacific Decadal Oscilation","url":"https://www.academia.edu/Documents/in/Pacific_Decadal_Oscilation?f_ri=43335"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_16785075" data-work_id="16785075" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/16785075/Coastal_vulnerability_across_the_Pacific_dominated_by_El_Ni%C3%B1o_Southern_Oscillation">Coastal vulnerability across the Pacific dominated by El Niño/Southern Oscillation</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">To predict future coastal hazards, it is important to quantify any links between climate drivers and spatial patterns of coastal change. However, most studies of future coastal vulnerability do not account for the dynamic components of... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_16785075" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">To predict future coastal hazards, it is important to quantify any links between climate drivers and spatial patterns of<br />coastal change. However, most studies of future coastal vulnerability do not account for the dynamic components of coastal<br />water levels during storms, notably wave-driven processes, storm surges and seasonal water level anomalies, although<br />these components can add metres to water levels during extreme events. Here we synthesize multi-decadal, co-located<br />data assimilated between 1979 and 2012 that describe wave climate, local water levels and coastal change for 48 beaches<br />throughout the Pacific Ocean basin. We find that observed coastal erosion across the Pacific varies most closely with<br />El Niño/Southern Oscillation, with a smaller influence from the Southern Annular Mode and the Pacific North American<br />pattern. In the northern and southern Pacific Ocean, regional wave and water level anomalies are significantly correlated<br />to a suite of climate indices, particularly during boreal winter; conditions in the northeast Pacific Ocean are often opposite<br />to those in the western and southern Pacific. We conclude that, if projections for an increasing frequency of extreme El Niño<br />and La Niña events over the twenty-first century are confirmed, then populated regions on opposite sides of the Pacific Ocean<br />basin could be alternately exposed to extreme coastal erosion and flooding, independent of sea-level rise.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/16785075" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="5f2404974d3793e9395c680a073276f8" rel="nofollow" data-download="{"attachment_id":39181306,"asset_id":16785075,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/39181306/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="11962699" href="https://ucsb.academia.edu/IanWalker">Ian J Walker</a><script data-card-contents-for-user="11962699" type="text/json">{"id":11962699,"first_name":"Ian","last_name":"Walker","domain_name":"ucsb","page_name":"IanWalker","display_name":"Ian J Walker","profile_url":"https://ucsb.academia.edu/IanWalker?f_ri=43335","photo":"https://0.academia-photos.com/11962699/3437185/4041511/s65_ian.walker.jpg"}</script></span></span></li><li class="js-paper-rank-work_16785075 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="16785075"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 16785075, container: ".js-paper-rank-work_16785075", }); });</script></li><li class="js-percentile-work_16785075 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 16785075; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_16785075"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_16785075 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="16785075"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 16785075; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=16785075]").text(description); $(".js-view-count-work_16785075").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_16785075").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="16785075"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">13</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="1275" href="https://www.academia.edu/Documents/in/Coastal_Management">Coastal Management</a>, <script data-card-contents-for-ri="1275" type="text/json">{"id":1275,"name":"Coastal Management","url":"https://www.academia.edu/Documents/in/Coastal_Management?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="1512" href="https://www.academia.edu/Documents/in/Climate_Change">Climate Change</a>, <script data-card-contents-for-ri="1512" type="text/json">{"id":1512,"name":"Climate Change","url":"https://www.academia.edu/Documents/in/Climate_Change?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="2637" href="https://www.academia.edu/Documents/in/Coastal_Processes">Coastal Processes</a>, <script data-card-contents-for-ri="2637" type="text/json">{"id":2637,"name":"Coastal Processes","url":"https://www.academia.edu/Documents/in/Coastal_Processes?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="4753" href="https://www.academia.edu/Documents/in/Climate_variability">Climate variability</a><script data-card-contents-for-ri="4753" type="text/json">{"id":4753,"name":"Climate variability","url":"https://www.academia.edu/Documents/in/Climate_variability?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=16785075]'), work: {"id":16785075,"title":"Coastal vulnerability across the Pacific dominated by El Niño/Southern Oscillation","created_at":"2015-10-14T08:30:46.691-07:00","url":"https://www.academia.edu/16785075/Coastal_vulnerability_across_the_Pacific_dominated_by_El_Ni%C3%B1o_Southern_Oscillation?f_ri=43335","dom_id":"work_16785075","summary":"To predict future coastal hazards, it is important to quantify any links between climate drivers and spatial patterns of\ncoastal change. However, most studies of future coastal vulnerability do not account for the dynamic components of coastal\nwater levels during storms, notably wave-driven processes, storm surges and seasonal water level anomalies, although\nthese components can add metres to water levels during extreme events. Here we synthesize multi-decadal, co-located\ndata assimilated between 1979 and 2012 that describe wave climate, local water levels and coastal change for 48 beaches\nthroughout the Pacific Ocean basin. We find that observed coastal erosion across the Pacific varies most closely with\nEl Niño/Southern Oscillation, with a smaller influence from the Southern Annular Mode and the Pacific North American\npattern. In the northern and southern Pacific Ocean, regional wave and water level anomalies are significantly correlated\nto a suite of climate indices, particularly during boreal winter; conditions in the northeast Pacific Ocean are often opposite\nto those in the western and southern Pacific. We conclude that, if projections for an increasing frequency of extreme El Niño\nand La Niña events over the twenty-first century are confirmed, then populated regions on opposite sides of the Pacific Ocean\nbasin could be alternately exposed to extreme coastal erosion and flooding, independent of sea-level rise.","downloadable_attachments":[{"id":39181306,"asset_id":16785075,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":11962699,"first_name":"Ian","last_name":"Walker","domain_name":"ucsb","page_name":"IanWalker","display_name":"Ian J Walker","profile_url":"https://ucsb.academia.edu/IanWalker?f_ri=43335","photo":"https://0.academia-photos.com/11962699/3437185/4041511/s65_ian.walker.jpg"}],"research_interests":[{"id":1275,"name":"Coastal Management","url":"https://www.academia.edu/Documents/in/Coastal_Management?f_ri=43335","nofollow":false},{"id":1512,"name":"Climate Change","url":"https://www.academia.edu/Documents/in/Climate_Change?f_ri=43335","nofollow":false},{"id":2637,"name":"Coastal Processes","url":"https://www.academia.edu/Documents/in/Coastal_Processes?f_ri=43335","nofollow":false},{"id":4753,"name":"Climate variability","url":"https://www.academia.edu/Documents/in/Climate_variability?f_ri=43335","nofollow":false},{"id":7827,"name":"Coastal Dunes","url":"https://www.academia.edu/Documents/in/Coastal_Dunes?f_ri=43335"},{"id":27086,"name":"Coastal Erosion","url":"https://www.academia.edu/Documents/in/Coastal_Erosion?f_ri=43335"},{"id":40999,"name":"El Niño","url":"https://www.academia.edu/Documents/in/El_Ni%C3%B1o?f_ri=43335"},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335"},{"id":126506,"name":"Sea-Level Rise","url":"https://www.academia.edu/Documents/in/Sea-Level_Rise?f_ri=43335"},{"id":149686,"name":"Wave and Storm Surge Modelling","url":"https://www.academia.edu/Documents/in/Wave_and_Storm_Surge_Modelling?f_ri=43335"},{"id":352631,"name":"Coastal Flood Hazards","url":"https://www.academia.edu/Documents/in/Coastal_Flood_Hazards?f_ri=43335"},{"id":376098,"name":"El Nino-Southern Oscillation","url":"https://www.academia.edu/Documents/in/El_Nino-Southern_Oscillation?f_ri=43335"},{"id":1150373,"name":"Pacific Decadal Oscilation","url":"https://www.academia.edu/Documents/in/Pacific_Decadal_Oscilation?f_ri=43335"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_1079557" data-work_id="1079557" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/1079557/Degradation_of_littoral_habitats_by_residential_development_woody_debris_in_lakes_of_the_Pacific_Northwest_and_Midwest_United_States">Degradation of littoral habitats by residential development: woody debris in lakes of the Pacific Northwest and Midwest, United States</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/1079557" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="8174e021c1545822f14db9da2107105c" rel="nofollow" data-download="{"attachment_id":11753682,"asset_id":1079557,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/11753682/download_file?st=MTczMjgyMzAzNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="930408" href="https://tacoma-washington.academia.edu/TessaFrancis">Tessa Francis</a><script data-card-contents-for-user="930408" type="text/json">{"id":930408,"first_name":"Tessa","last_name":"Francis","domain_name":"tacoma-washington","page_name":"TessaFrancis","display_name":"Tessa Francis","profile_url":"https://tacoma-washington.academia.edu/TessaFrancis?f_ri=43335","photo":"https://0.academia-photos.com/930408/434513/11792874/s65_tessa.francis.jpg"}</script></span></span></li><li class="js-paper-rank-work_1079557 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="1079557"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 1079557, container: ".js-paper-rank-work_1079557", }); });</script></li><li class="js-percentile-work_1079557 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 1079557; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_1079557"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_1079557 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="1079557"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 1079557; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=1079557]").text(description); $(".js-view-count-work_1079557").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_1079557").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="1079557"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">4</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="1999" href="https://www.academia.edu/Documents/in/Limnology">Limnology</a>, <script data-card-contents-for-ri="1999" type="text/json">{"id":1999,"name":"Limnology","url":"https://www.academia.edu/Documents/in/Limnology?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="11278" href="https://www.academia.edu/Documents/in/Urban_Ecology">Urban Ecology</a>, <script data-card-contents-for-ri="11278" type="text/json">{"id":11278,"name":"Urban Ecology","url":"https://www.academia.edu/Documents/in/Urban_Ecology?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="43335" href="https://www.academia.edu/Documents/in/Shoreline_Management_Planning">Shoreline Management Planning</a>, <script data-card-contents-for-ri="43335" type="text/json">{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="224646" href="https://www.academia.edu/Documents/in/Shoreline_Dynamics">Shoreline Dynamics</a><script data-card-contents-for-ri="224646" type="text/json">{"id":224646,"name":"Shoreline Dynamics","url":"https://www.academia.edu/Documents/in/Shoreline_Dynamics?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=1079557]'), work: {"id":1079557,"title":"Degradation of littoral habitats by residential development: woody debris in lakes of the Pacific Northwest and Midwest, United States","created_at":"2011-11-10T03:28:51.761-08:00","url":"https://www.academia.edu/1079557/Degradation_of_littoral_habitats_by_residential_development_woody_debris_in_lakes_of_the_Pacific_Northwest_and_Midwest_United_States?f_ri=43335","dom_id":"work_1079557","summary":null,"downloadable_attachments":[{"id":11753682,"asset_id":1079557,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":930408,"first_name":"Tessa","last_name":"Francis","domain_name":"tacoma-washington","page_name":"TessaFrancis","display_name":"Tessa Francis","profile_url":"https://tacoma-washington.academia.edu/TessaFrancis?f_ri=43335","photo":"https://0.academia-photos.com/930408/434513/11792874/s65_tessa.francis.jpg"}],"research_interests":[{"id":1999,"name":"Limnology","url":"https://www.academia.edu/Documents/in/Limnology?f_ri=43335","nofollow":false},{"id":11278,"name":"Urban Ecology","url":"https://www.academia.edu/Documents/in/Urban_Ecology?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false},{"id":224646,"name":"Shoreline Dynamics","url":"https://www.academia.edu/Documents/in/Shoreline_Dynamics?f_ri=43335","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_536539" data-work_id="536539" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/536539/Quantifying_thresholds_for_significant_dune_erosion_along_the_Sefton_Coast_Northwest_England">Quantifying thresholds for significant dune erosion along the Sefton Coast, Northwest England </a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">"Field and model hindcast data are used to establish a critical dune erosion threshold for the Sefton Coast (NW England). Events are classified as causing significant erosion if they result in: (a) a mean dune retreat along the entire... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_536539" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">"Field and model hindcast data are used to establish a critical dune erosion threshold for the Sefton Coast (NW England). Events are classified as causing significant erosion if they result in: (a) a mean dune retreat along the entire study area of > 2 m; (b) a dune retreat of ≥ 5 m along a coastal segment ≥ 2 km in length; and (c) an eroded area ≥ 20,000 m2. For the period 1996 to 2008, individual storms were characterised using hindcast results from a POLCOMS-WAM model and measured data from the Liverpool Bay Coastal Observatory. Results show that combined extreme surge levels (> 1.5 m) and wave heights (> 4 m), or tidal water levels above 9.0 m Chart Datum (CD), do not always result in significant dune erosion. Evidence suggests that erosion is more likely to occur when wave heights are > 2.6 m, peak water level is > 10.2 m CD at Liverpool and when consecutive tidal cycles provide 10 h or more of water levels above 9.4 m CD. However, lower water levels and wave heights, and shorter events of sustained water levels, can cause significant erosion in the summer. While the return period for events giving rise to the most severe erosion in the winter is > 50 years, significant erosion in the summer can be caused by events with return periods < 1 year. It is suggested that this may be attributable to a known reduction in the mean dune toe elevation c. 30 cm. Although the study shows it might be possible to characterise objectively storm events based on oceanographic conditions, the resultant morphological change at the coast is demonstrated to depend on the time and duration of events, and on other variables which are not so easy to quantify. Further investigation is needed to understand the influence of alongshore and seasonal variability in beach/dune morphology in determining the response to the hydrodynamic and meteorological conditions causing significant erosion. Improved monitoring pre- and post-storm of changes in beach/dune morphology is required to develop reliable proxies that can be used to establish early warning systems to mitigate the impacts of erosion and flooding in the future. <br /> <br />"</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/536539" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="93265" href="https://bournemouth.academia.edu/LucianaEsteves">Luciana Esteves</a><script data-card-contents-for-user="93265" type="text/json">{"id":93265,"first_name":"Luciana","last_name":"Esteves","domain_name":"bournemouth","page_name":"LucianaEsteves","display_name":"Luciana Esteves","profile_url":"https://bournemouth.academia.edu/LucianaEsteves?f_ri=43335","photo":"https://0.academia-photos.com/93265/25858/23849/s65_luciana.esteves.jpg"}</script></span></span></li><li class="js-paper-rank-work_536539 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="536539"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 536539, container: ".js-paper-rank-work_536539", }); });</script></li><li class="js-percentile-work_536539 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 536539; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_536539"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_536539 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="536539"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 536539; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=536539]").text(description); $(".js-view-count-work_536539").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_536539").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="536539"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">13</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="281" href="https://www.academia.edu/Documents/in/Physical_Geography">Physical Geography</a>, <script data-card-contents-for-ri="281" type="text/json">{"id":281,"name":"Physical Geography","url":"https://www.academia.edu/Documents/in/Physical_Geography?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="1275" href="https://www.academia.edu/Documents/in/Coastal_Management">Coastal Management</a>, <script data-card-contents-for-ri="1275" type="text/json">{"id":1275,"name":"Coastal Management","url":"https://www.academia.edu/Documents/in/Coastal_Management?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="2637" href="https://www.academia.edu/Documents/in/Coastal_Processes">Coastal Processes</a>, <script data-card-contents-for-ri="2637" type="text/json">{"id":2637,"name":"Coastal Processes","url":"https://www.academia.edu/Documents/in/Coastal_Processes?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="6807" href="https://www.academia.edu/Documents/in/Coastal_Geography">Coastal Geography</a><script data-card-contents-for-ri="6807" type="text/json">{"id":6807,"name":"Coastal Geography","url":"https://www.academia.edu/Documents/in/Coastal_Geography?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=536539]'), work: {"id":536539,"title":"Quantifying thresholds for significant dune erosion along the Sefton Coast, Northwest England ","created_at":"2011-04-18T16:39:36.008-07:00","url":"https://www.academia.edu/536539/Quantifying_thresholds_for_significant_dune_erosion_along_the_Sefton_Coast_Northwest_England?f_ri=43335","dom_id":"work_536539","summary":"\"Field and model hindcast data are used to establish a critical dune erosion threshold for the Sefton Coast (NW England). Events are classified as causing significant erosion if they result in: (a) a mean dune retreat along the entire study area of \u003e 2 m; (b) a dune retreat of ≥ 5 m along a coastal segment ≥ 2 km in length; and (c) an eroded area ≥ 20,000 m2. For the period 1996 to 2008, individual storms were characterised using hindcast results from a POLCOMS-WAM model and measured data from the Liverpool Bay Coastal Observatory. Results show that combined extreme surge levels (\u003e 1.5 m) and wave heights (\u003e 4 m), or tidal water levels above 9.0 m Chart Datum (CD), do not always result in significant dune erosion. Evidence suggests that erosion is more likely to occur when wave heights are \u003e 2.6 m, peak water level is \u003e 10.2 m CD at Liverpool and when consecutive tidal cycles provide 10 h or more of water levels above 9.4 m CD. However, lower water levels and wave heights, and shorter events of sustained water levels, can cause significant erosion in the summer. While the return period for events giving rise to the most severe erosion in the winter is \u003e 50 years, significant erosion in the summer can be caused by events with return periods \u003c 1 year. It is suggested that this may be attributable to a known reduction in the mean dune toe elevation c. 30 cm. Although the study shows it might be possible to characterise objectively storm events based on oceanographic conditions, the resultant morphological change at the coast is demonstrated to depend on the time and duration of events, and on other variables which are not so easy to quantify. Further investigation is needed to understand the influence of alongshore and seasonal variability in beach/dune morphology in determining the response to the hydrodynamic and meteorological conditions causing significant erosion. Improved monitoring pre- and post-storm of changes in beach/dune morphology is required to develop reliable proxies that can be used to establish early warning systems to mitigate the impacts of erosion and flooding in the future.\r\n\r\n\"","downloadable_attachments":[],"ordered_authors":[{"id":93265,"first_name":"Luciana","last_name":"Esteves","domain_name":"bournemouth","page_name":"LucianaEsteves","display_name":"Luciana Esteves","profile_url":"https://bournemouth.academia.edu/LucianaEsteves?f_ri=43335","photo":"https://0.academia-photos.com/93265/25858/23849/s65_luciana.esteves.jpg"}],"research_interests":[{"id":281,"name":"Physical Geography","url":"https://www.academia.edu/Documents/in/Physical_Geography?f_ri=43335","nofollow":false},{"id":1275,"name":"Coastal Management","url":"https://www.academia.edu/Documents/in/Coastal_Management?f_ri=43335","nofollow":false},{"id":2637,"name":"Coastal Processes","url":"https://www.academia.edu/Documents/in/Coastal_Processes?f_ri=43335","nofollow":false},{"id":6807,"name":"Coastal Geography","url":"https://www.academia.edu/Documents/in/Coastal_Geography?f_ri=43335","nofollow":false},{"id":6808,"name":"Coastal Geomorphology","url":"https://www.academia.edu/Documents/in/Coastal_Geomorphology?f_ri=43335"},{"id":7827,"name":"Coastal Dunes","url":"https://www.academia.edu/Documents/in/Coastal_Dunes?f_ri=43335"},{"id":25439,"name":"Coastal geomorphology (Earth Sciences)","url":"https://www.academia.edu/Documents/in/Coastal_geomorphology_Earth_Sciences_?f_ri=43335"},{"id":27086,"name":"Coastal Erosion","url":"https://www.academia.edu/Documents/in/Coastal_Erosion?f_ri=43335"},{"id":40021,"name":"Coastal Zone Management","url":"https://www.academia.edu/Documents/in/Coastal_Zone_Management?f_ri=43335"},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335"},{"id":98736,"name":"digital cartography, GIS, physical geography","url":"https://www.academia.edu/Documents/in/digital_cartography_GIS_physical_geography?f_ri=43335"},{"id":247805,"name":"Storm Impact","url":"https://www.academia.edu/Documents/in/Storm_Impact?f_ri=43335"},{"id":247806,"name":"Shoreline Change","url":"https://www.academia.edu/Documents/in/Shoreline_Change?f_ri=43335"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_199971" data-work_id="199971" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/199971/Quantifying_Shoreline_Changes_along_the_Sefton_Coast_UK_and_the_Implications_for_Research_Informed_Coastal_Management">Quantifying Shoreline Changes along the Sefton Coast (UK) and the Implications for Research-Informed Coastal Management</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The Sefton coast is a 36-km long coastline located between the Mersey and the Ribble estuaries in northwest England. It encompasses the longest coastal dune system in England and Wales, which has been rapidly eroding in the last century.... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_199971" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The Sefton coast is a 36-km long coastline located between the Mersey and the Ribble estuaries in northwest England. It encompasses the longest coastal dune system in England and Wales, which has been rapidly eroding in the last century. The arcuate shape of this coast favours erosion at the prominent shore of Formby Point from where sediment diverges and is transported longshore promoting accretion northwards and southwards. This study aims to assess how different ways of estimating shoreline change rates (using different proxies and statistical methods) can affect future predictions of shoreline positions. Coastline and high water line positions, dune toe surveys and beach profiles spanning different time frames are analysed. Shoreline change rates are highly dependent on the proxy used to map the shoreline and the statistical methods used to estimate rates of changes. Generic models to predict future positions of the shoreline do not produce good results for this study area. Therefore, the analysis of long-term and a regular monitoring of various shoreline proxies are the best alternative for predicting future shoreline positions. An improved understanding of the past and present patterns of shoreline changes at different spatial and time scales is necessary to support best management practices taking into account scenarios of climate change.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/199971" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="93265" href="https://bournemouth.academia.edu/LucianaEsteves">Luciana Esteves</a><script data-card-contents-for-user="93265" type="text/json">{"id":93265,"first_name":"Luciana","last_name":"Esteves","domain_name":"bournemouth","page_name":"LucianaEsteves","display_name":"Luciana Esteves","profile_url":"https://bournemouth.academia.edu/LucianaEsteves?f_ri=43335","photo":"https://0.academia-photos.com/93265/25858/23849/s65_luciana.esteves.jpg"}</script></span></span></li><li class="js-paper-rank-work_199971 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="199971"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 199971, container: ".js-paper-rank-work_199971", }); });</script></li><li class="js-percentile-work_199971 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 199971; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_199971"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_199971 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="199971"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 199971; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=199971]").text(description); $(".js-view-count-work_199971").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_199971").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="199971"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">4</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="23056" href="https://www.academia.edu/Documents/in/Geo-spatial_analysis_with_GIS_and_GPS">Geo-spatial analysis with GIS and GPS</a>, <script data-card-contents-for-ri="23056" type="text/json">{"id":23056,"name":"Geo-spatial analysis with GIS and GPS","url":"https://www.academia.edu/Documents/in/Geo-spatial_analysis_with_GIS_and_GPS?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="27086" href="https://www.academia.edu/Documents/in/Coastal_Erosion">Coastal Erosion</a>, <script data-card-contents-for-ri="27086" type="text/json">{"id":27086,"name":"Coastal Erosion","url":"https://www.academia.edu/Documents/in/Coastal_Erosion?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="43335" href="https://www.academia.edu/Documents/in/Shoreline_Management_Planning">Shoreline Management Planning</a>, <script data-card-contents-for-ri="43335" type="text/json">{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="1009312" href="https://www.academia.edu/Documents/in/Geographic_Information_Systems_GIS_">Geographic Information Systems (GIS)</a><script data-card-contents-for-ri="1009312" type="text/json">{"id":1009312,"name":"Geographic Information Systems (GIS)","url":"https://www.academia.edu/Documents/in/Geographic_Information_Systems_GIS_?f_ri=43335","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=199971]'), work: {"id":199971,"title":"Quantifying Shoreline Changes along the Sefton Coast (UK) and the Implications for Research-Informed Coastal Management","created_at":"2009-12-01T18:56:49.712-08:00","url":"https://www.academia.edu/199971/Quantifying_Shoreline_Changes_along_the_Sefton_Coast_UK_and_the_Implications_for_Research_Informed_Coastal_Management?f_ri=43335","dom_id":"work_199971","summary":"The Sefton coast is a 36-km long coastline located between the Mersey and the Ribble estuaries in northwest England. It encompasses the longest coastal dune system in England and Wales, which has been rapidly eroding in the last century. The arcuate shape of this coast favours erosion at the prominent shore of Formby Point from where sediment diverges and is transported longshore promoting accretion northwards and southwards. This study aims to assess how different ways of estimating shoreline change rates (using different proxies and statistical methods) can affect future predictions of shoreline positions. Coastline and high water line positions, dune toe surveys and beach profiles spanning different time frames are analysed. Shoreline change rates are highly dependent on the proxy used to map the shoreline and the statistical methods used to estimate rates of changes. Generic models to predict future positions of the shoreline do not produce good results for this study area. Therefore, the analysis of long-term and a regular monitoring of various shoreline proxies are the best alternative for predicting future shoreline positions. An improved understanding of the past and present patterns of shoreline changes at different spatial and time scales is necessary to support best management practices taking into account scenarios of climate change.","downloadable_attachments":[],"ordered_authors":[{"id":93265,"first_name":"Luciana","last_name":"Esteves","domain_name":"bournemouth","page_name":"LucianaEsteves","display_name":"Luciana Esteves","profile_url":"https://bournemouth.academia.edu/LucianaEsteves?f_ri=43335","photo":"https://0.academia-photos.com/93265/25858/23849/s65_luciana.esteves.jpg"}],"research_interests":[{"id":23056,"name":"Geo-spatial analysis with GIS and GPS","url":"https://www.academia.edu/Documents/in/Geo-spatial_analysis_with_GIS_and_GPS?f_ri=43335","nofollow":false},{"id":27086,"name":"Coastal Erosion","url":"https://www.academia.edu/Documents/in/Coastal_Erosion?f_ri=43335","nofollow":false},{"id":43335,"name":"Shoreline Management Planning","url":"https://www.academia.edu/Documents/in/Shoreline_Management_Planning?f_ri=43335","nofollow":false},{"id":1009312,"name":"Geographic Information Systems (GIS)","url":"https://www.academia.edu/Documents/in/Geographic_Information_Systems_GIS_?f_ri=43335","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div></div><div class="u-taCenter Pagination"><ul class="pagination"></ul></div></div><div class="hidden-xs hidden-sm"><div class="u-pl6x"><div style="width: 300px;"><div class="panel panel-flat u-mt7x"><div class="panel-heading u-p5x"><div class="u-tcGrayDark u-taCenter u-fw700 u-textUppercase">Related Topics</div></div><ul class="list-group"><li class="list-group-item media_v2 u-mt0x u-p3x"><div class="media-body"><div class="u-tcGrayDarker u-fw700"><a class="u-tcGrayDarker" href="https://www.academia.edu/Documents/in/Cities_and_globalization_Global_cities">Cities and globalization/Global cities</a></div></div><div class="media-right media-middle"><a 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