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js-section-heading" data-section="Papers" id="Papers"><h3 class="profile--tab_heading_container">Papers by Jacques Piazzola</h3></div><div class="js-work-strip profile--work_container" data-work-id="93272081"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/93272081/Les_%C3%AEles_d_Hy%C3%A8res_dans_le_syst%C3%A8me_de_circulation_marine_et_atmosph%C3%A9rique_de_la_M%C3%A9diterran%C3%A9e"><img alt="Research paper thumbnail of Les îles d’Hyères dans le système de circulation marine et atmosphérique de la Méditerranée" class="work-thumbnail" src="https://attachments.academia-assets.com/96055012/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/93272081/Les_%C3%AEles_d_Hy%C3%A8res_dans_le_syst%C3%A8me_de_circulation_marine_et_atmosph%C3%A9rique_de_la_M%C3%A9diterran%C3%A9e">Les îles d’Hyères dans le système de circulation marine et atmosphérique de la Méditerranée</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Cet article a pour but de présenter les grandes lignes du fonctionnement de la circulation marine...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Cet article a pour but de présenter les grandes lignes du fonctionnement de la circulation marine et atmosphérique de la Méditerranée, afin de mieux comprendre les phénomènes physiques qui affectent les îles d'Hyères, d'optimiser la gestion de leur environnement et le cas 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class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/93272080/Development_of_a_sea_salt_emission_parameterization_for_the_North_western_Mediterranean"><img alt="Research paper thumbnail of Development of a sea salt emission parameterization for the North-western Mediterranean" class="work-thumbnail" src="https://attachments.academia-assets.com/96055008/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/93272080/Development_of_a_sea_salt_emission_parameterization_for_the_North_western_Mediterranean">Development of a sea salt emission parameterization for the North-western Mediterranean</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The aim of the present work is to determinate an accurate formulation for the sea-spray source fu...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The aim of the present work is to determinate an accurate formulation for the sea-spray source function issued from the bubble bursting processes. To this end, a simple aerosol transport Model, the Macmod Model (Tedeschi and Piazzola, 2011) was implemented in the Mediterranean area using different flux formulations for the sea spray source function (e.g., Demoisson et al., 2013; Gong et al., 2003; Monahan et al., 1986; Odvanevaite et al., 2014). The simulations were then compared to a large data set dealing with the aerosol size distributions acquired during an extensive series of measurements in the Northwestern Mediterranean. The results, which are part of an article that will be submitted soon, allowed determination of an accurate sea-spray source function formulation and its dependence on the wave development.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d1aa795168a8acd2cd2fed845e0ada2b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":96055008,"asset_id":93272080,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/96055008/download_file?st=MTczNzI0NDAzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="93272080"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="93272080"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 93272080; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=93272080]").text(description); $(".js-view-count[data-work-id=93272080]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 93272080; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='93272080']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 93272080, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "d1aa795168a8acd2cd2fed845e0ada2b" } } $('.js-work-strip[data-work-id=93272080]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":93272080,"title":"Development of a sea salt emission parameterization for the North-western Mediterranean","translated_title":"","metadata":{"abstract":"The aim of the present work is to determinate an accurate formulation for the sea-spray source function issued from the bubble bursting processes. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358690"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/79358690/Study_of_the_Impact_of_the_Natural_Production_of_Coastal_Marine_Aerosols_on_the_Dynamics_and_Microphysical_Behavior_of_a_Convective_Cloud"><img alt="Research paper thumbnail of Study of the Impact of the Natural Production of Coastal Marine Aerosols on the Dynamics and Microphysical Behavior of a Convective Cloud" class="work-thumbnail" src="https://attachments.academia-assets.com/86100613/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/79358690/Study_of_the_Impact_of_the_Natural_Production_of_Coastal_Marine_Aerosols_on_the_Dynamics_and_Microphysical_Behavior_of_a_Convective_Cloud">Study of the Impact of the Natural Production of Coastal Marine Aerosols on the Dynamics and Microphysical Behavior of a Convective Cloud</a></div><div class="wp-workCard_item"><span>IEEE Geoscience and Remote Sensing Letters</span><span>, 2013</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The atmosphere contains suspended particles of various origins natural or anthropogenic that cons...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The atmosphere contains suspended particles of various origins natural or anthropogenic that constitutes the atmospheric aerosol. The aerosol cloud interaction is a fundamental mechanis m that influences the precipitation process. To study the impact of ma rine aerosols, especially those generated in coastal areas, on the dynamics and microphysical behavior of the clouds, two numerical models were coupled. The first, calculates the coastal ma rine aerosol spectrum that could be generated under a given weather condition at the sea surface. The p redicted spectrum is then introduced, as in itial aerosol spectra, to a cloud model with a detailed microphysics. The simulat ions performed have focused on a convective cloud (mixed phase) using distinct initial aerosols spectra of different origins in order to highlight the potential effect of ma rine aerosol naturally produced in surf zone on the dynamics and microphysics of the cloud. The results carried out indicates an important contribution of marine aerosol in the process of precipitation formation by promoting an early start of precipitat ion at lower alt itudes, leading to increased amounts of precipitation reaching the ground.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="bd1d964b1f01880521feb663b998e43b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100613,"asset_id":79358690,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100613/download_file?st=MTczNzI0NDAzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358690"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358690"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358690; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358690]").text(description); $(".js-view-count[data-work-id=79358690]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358690; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358690']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358690, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "bd1d964b1f01880521feb663b998e43b" } } $('.js-work-strip[data-work-id=79358690]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358690,"title":"Study of the Impact of the Natural Production of Coastal Marine Aerosols on the Dynamics and Microphysical Behavior of a Convective Cloud","translated_title":"","metadata":{"publisher":"Institute of Electrical and Electronics Engineers","grobid_abstract":"The atmosphere contains suspended particles of various origins natural or anthropogenic that constitutes the atmospheric aerosol. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358623"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/79358623/Sea_spray_aerosols_and_SARS_Cov_2_an_analysis_using_AERONET_data"><img alt="Research paper thumbnail of Sea-spray aerosols and SARS-Cov-2: an analysis using AERONET data" class="work-thumbnail" src="https://attachments.academia-assets.com/86100558/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/79358623/Sea_spray_aerosols_and_SARS_Cov_2_an_analysis_using_AERONET_data">Sea-spray aerosols and SARS-Cov-2: an analysis using AERONET data</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Even if the people density, habits and displacements probably represent the most important causes...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Even if the people density, habits and displacements probably represent the most important causes of the SARS-Cov-2 virus propagation, the role of the atmospheric aerosol in COVID-19 outbreaks is significant and it needs to be further investigated. Therefore, we aimed to study if the aerosol properties related to the different sources and meteorological conditions we can observe in continental and coastal urbanized areas can have an influence on the atmospheric transport of the SARS-Cov-2 virus. This paper focuses on the lockdown period to reduce the differences in the social behavior. As an example, we investigated the contamination cases during March 2020 in two specific French areas located in both continental and coastal areas with regard to the meteorological conditions and the corresponding aerosol properties. To this end, we used both the optical depth (AOD) and the Angstrom exponent provided by the AERONET network. The results show that the analysis of aerosol ground-based d...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="409eeed45e9fbdc1e1dd09affa93592f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100558,"asset_id":79358623,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100558/download_file?st=MTczNzI0NDAzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358623"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358623"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358623; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358623]").text(description); $(".js-view-count[data-work-id=79358623]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358623; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358623']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358623, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "409eeed45e9fbdc1e1dd09affa93592f" } } $('.js-work-strip[data-work-id=79358623]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358623,"title":"Sea-spray aerosols and SARS-Cov-2: an analysis using AERONET data","translated_title":"","metadata":{"abstract":"Even if the people density, habits and displacements probably represent the most important causes of the SARS-Cov-2 virus propagation, the role of the atmospheric aerosol in COVID-19 outbreaks is significant and it needs to be further investigated. 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The model that is most frequently used for the prediction of aerosols and their effect on extinction in the marine atmosphere is the US Navy Aerosol Model (NAM). However, NAM can be significantly less reliable in coastal areas than on the open ocean. Based on an extensive series of measurements conducted on the island of Inisheer (Irish West Coast), an empirical aerosol model for the coastal zone formulated as an extension of NAM, in which coastal effects are modeled as a function of fetch, has been developed. This work is extended to the Mediterranean using an aerosol dataset recorded on the island of Porquerolles in the Bay of Toulon (France) and has been coupled with the Mie theory to give a code for the extinction, the code MEDiterranean EXtinction (MEDEX).</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2e666c0e715c1953a002d848d01dfe24" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100535,"asset_id":79358592,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100535/download_file?st=MTczNzI0NDAzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358592"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358592"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358592; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358592]").text(description); $(".js-view-count[data-work-id=79358592]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358592; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358592']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358592, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "2e666c0e715c1953a002d848d01dfe24" } } $('.js-work-strip[data-work-id=79358592]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358592,"title":"Development of the Mediterranean extinction code (MEDEX)","translated_title":"","metadata":{"publisher":"SPIE-Intl Soc Optical Eng","grobid_abstract":"The performance of electro-optical systems can be substantially affected by aerosol particles that scatter and absorb electromagnetic radiation. 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In particular, it is well recognized that the whitecap cover induced by breaking waves allows substantial enhancement of heat, momentum, gas and particle transfer at the air-sea interface. A large number of studies were conducted during the last decades on the variation of the whitecap fraction, commonly noted W. The results presented in this paper deal with the evolution of the whitecap coverage in coastal zone. In such areas, the wave field is often unsteady with an important variety of sea state developments. The present analysis is based on an extensive series of data obtained during an experimental campaign which took place on the Mediterranean coast in 2001. The results allow observation of the influence of the sea state conditions of the wave field on the whitecap coverage. In addition, this paper confirms the occurrence of a peak in the variations of the whitecap fraction with the wave age for coastal areas as suggested by Lafon et al. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358542"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/79358542/Variations_of_the_aerosol_concentration_with_fetch"><img alt="Research paper thumbnail of Variations of the aerosol concentration with fetch" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/79358542/Variations_of_the_aerosol_concentration_with_fetch">Variations of the aerosol concentration with fetch</a></div><div class="wp-workCard_item"><span>Journal of Aerosol Science</span><span>, 1999</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358542"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358542"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358542; 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=79358542]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358542,"title":"Variations of the aerosol concentration with fetch","translated_title":"","metadata":{"publisher":"Elsevier BV","publication_date":{"day":null,"month":null,"year":1999,"errors":{}},"publication_name":"Journal of Aerosol Science"},"translated_abstract":null,"internal_url":"https://www.academia.edu/79358542/Variations_of_the_aerosol_concentration_with_fetch","translated_internal_url":"","created_at":"2022-05-18T00:55:46.879-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":40419649,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Variations_of_the_aerosol_concentration_with_fetch","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":null,"owner":{"id":40419649,"first_name":"Jacques","middle_initials":"","last_name":"Piazzola","page_name":"JacquesPiazzola","domain_name":"independent","created_at":"2015-12-20T02:11:32.317-08:00","display_name":"Jacques Piazzola","url":"https://independent.academia.edu/JacquesPiazzola"},"attachments":[],"research_interests":[{"id":72,"name":"Chemical Engineering","url":"https://www.academia.edu/Documents/in/Chemical_Engineering"},{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences"},{"id":1759667,"name":"Aerosol Science","url":"https://www.academia.edu/Documents/in/Aerosol_Science"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358540"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/79358540/Characterization_of_carbonaceous_aerosols_over_Delhi_in_Ganga_basin_seasonal_variability_and_possible_sources"><img alt="Research paper thumbnail of Characterization of carbonaceous aerosols over Delhi in Ganga basin: seasonal variability and possible sources" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/79358540/Characterization_of_carbonaceous_aerosols_over_Delhi_in_Ganga_basin_seasonal_variability_and_possible_sources">Characterization of carbonaceous aerosols over Delhi in Ganga basin: seasonal variability and possible sources</a></div><div class="wp-workCard_item"><span>Environmental Science and Pollution Research</span><span>, 2014</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The mass concentration of carbonaceous species, organic carbon (OC), and elemental carbon (EC) us...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The mass concentration of carbonaceous species, organic carbon (OC), and elemental carbon (EC) using a semicontinuous thermo-optical EC-OC analyzer, and black carbon (BC) using an Aethalometer were measured simultaneously at an urban mega city Delhi in Ganga basin from January 2011 to May 2012. The concentrations of OC, EC, and BC exhibit seasonal variability, and their concentrations were ∼2 times higher during winter (OC 38.1 ± 17.9 μg m(-3), EC 15.8 ± 7.3 μg m(-3), and BC 10.1 ± 5.3 μg m(-3)) compared to those in summer (OC 14.1 ± 4.3 μg m(-3), EC 7.5 ± 1.5 μg m(-3), and BC 4.9 ± 1.5 μg m(-3)). A significant correlation between OC and EC (R = 0.95, n = 232) indicate their common emission sources with relatively lower OC/EC ratio (range 1.0-3.6, mean 2.2 ± 0.5) suggests fossil fuel emission as a major source of carbonaceous aerosols over the station. On average, mass concentration of EC was found to be ∼38 % higher than BC during the study period. The measured absorption coefficient (babs) was significantly correlated with EC, suggesting EC as a major absorbing species in ambient aerosols at Delhi. Furthermore, the estimated mass absorption efficiency (σabs) values are similar during winter (5.0 ± 1.5 m(2) g(-1)) and summer (4.8 ± 2.8 m(2) g(-1)). Significantly high aerosol loading of carbonaceous species emphasize an urgent need to focus on air quality management and proper impact assessment on health perspective in these regions.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358540"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358540"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358540; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358540]").text(description); $(".js-view-count[data-work-id=79358540]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358540; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358540']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358540, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=79358540]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358540,"title":"Characterization of carbonaceous aerosols over Delhi in Ganga basin: seasonal variability and possible sources","translated_title":"","metadata":{"abstract":"The mass concentration of carbonaceous species, organic carbon (OC), and elemental carbon (EC) using a semicontinuous thermo-optical EC-OC analyzer, and black carbon (BC) using an Aethalometer were measured simultaneously at an urban mega city Delhi in Ganga basin from January 2011 to May 2012. The concentrations of OC, EC, and BC exhibit seasonal variability, and their concentrations were ∼2 times higher during winter (OC 38.1 ± 17.9 μg m(-3), EC 15.8 ± 7.3 μg m(-3), and BC 10.1 ± 5.3 μg m(-3)) compared to those in summer (OC 14.1 ± 4.3 μg m(-3), EC 7.5 ± 1.5 μg m(-3), and BC 4.9 ± 1.5 μg m(-3)). A significant correlation between OC and EC (R = 0.95, n = 232) indicate their common emission sources with relatively lower OC/EC ratio (range 1.0-3.6, mean 2.2 ± 0.5) suggests fossil fuel emission as a major source of carbonaceous aerosols over the station. On average, mass concentration of EC was found to be ∼38 % higher than BC during the study period. The measured absorption coefficient (babs) was significantly correlated with EC, suggesting EC as a major absorbing species in ambient aerosols at Delhi. Furthermore, the estimated mass absorption efficiency (σabs) values are similar during winter (5.0 ± 1.5 m(2) g(-1)) and summer (4.8 ± 2.8 m(2) g(-1)). Significantly high aerosol loading of carbonaceous species emphasize an urgent need to focus on air quality management and proper impact assessment on health perspective in these regions.","publisher":"Springer Nature","publication_date":{"day":null,"month":null,"year":2014,"errors":{}},"publication_name":"Environmental Science and Pollution Research"},"translated_abstract":"The mass concentration of carbonaceous species, organic carbon (OC), and elemental carbon (EC) using a semicontinuous thermo-optical EC-OC analyzer, and black carbon (BC) using an Aethalometer were measured simultaneously at an urban mega city Delhi in Ganga basin from January 2011 to May 2012. The concentrations of OC, EC, and BC exhibit seasonal variability, and their concentrations were ∼2 times higher during winter (OC 38.1 ± 17.9 μg m(-3), EC 15.8 ± 7.3 μg m(-3), and BC 10.1 ± 5.3 μg m(-3)) compared to those in summer (OC 14.1 ± 4.3 μg m(-3), EC 7.5 ± 1.5 μg m(-3), and BC 4.9 ± 1.5 μg m(-3)). A significant correlation between OC and EC (R = 0.95, n = 232) indicate their common emission sources with relatively lower OC/EC ratio (range 1.0-3.6, mean 2.2 ± 0.5) suggests fossil fuel emission as a major source of carbonaceous aerosols over the station. On average, mass concentration of EC was found to be ∼38 % higher than BC during the study period. The measured absorption coefficient (babs) was significantly correlated with EC, suggesting EC as a major absorbing species in ambient aerosols at Delhi. Furthermore, the estimated mass absorption efficiency (σabs) values are similar during winter (5.0 ± 1.5 m(2) g(-1)) and summer (4.8 ± 2.8 m(2) g(-1)). Significantly high aerosol loading of carbonaceous species emphasize an urgent need to focus on air quality management and proper impact assessment on health perspective in these regions.","internal_url":"https://www.academia.edu/79358540/Characterization_of_carbonaceous_aerosols_over_Delhi_in_Ganga_basin_seasonal_variability_and_possible_sources","translated_internal_url":"","created_at":"2022-05-18T00:55:36.806-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":40419649,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Characterization_of_carbonaceous_aerosols_over_Delhi_in_Ganga_basin_seasonal_variability_and_possible_sources","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"The mass concentration of carbonaceous species, organic carbon (OC), and elemental carbon (EC) using a semicontinuous thermo-optical EC-OC analyzer, and black carbon (BC) using an Aethalometer were measured simultaneously at an urban mega city Delhi in Ganga basin from January 2011 to May 2012. The concentrations of OC, EC, and BC exhibit seasonal variability, and their concentrations were ∼2 times higher during winter (OC 38.1 ± 17.9 μg m(-3), EC 15.8 ± 7.3 μg m(-3), and BC 10.1 ± 5.3 μg m(-3)) compared to those in summer (OC 14.1 ± 4.3 μg m(-3), EC 7.5 ± 1.5 μg m(-3), and BC 4.9 ± 1.5 μg m(-3)). A significant correlation between OC and EC (R = 0.95, n = 232) indicate their common emission sources with relatively lower OC/EC ratio (range 1.0-3.6, mean 2.2 ± 0.5) suggests fossil fuel emission as a major source of carbonaceous aerosols over the station. On average, mass concentration of EC was found to be ∼38 % higher than BC during the study period. The measured absorption coefficient (babs) was significantly correlated with EC, suggesting EC as a major absorbing species in ambient aerosols at Delhi. Furthermore, the estimated mass absorption efficiency (σabs) values are similar during winter (5.0 ± 1.5 m(2) g(-1)) and summer (4.8 ± 2.8 m(2) g(-1)). Significantly high aerosol loading of carbonaceous species emphasize an urgent need to focus on air quality management and proper impact assessment on health perspective in these regions.","owner":{"id":40419649,"first_name":"Jacques","middle_initials":"","last_name":"Piazzola","page_name":"JacquesPiazzola","domain_name":"independent","created_at":"2015-12-20T02:11:32.317-08:00","display_name":"Jacques Piazzola","url":"https://independent.academia.edu/JacquesPiazzola"},"attachments":[],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":523,"name":"Chemistry","url":"https://www.academia.edu/Documents/in/Chemistry"},{"id":5303,"name":"Carbon","url":"https://www.academia.edu/Documents/in/Carbon"},{"id":11801,"name":"Environmental Monitoring","url":"https://www.academia.edu/Documents/in/Environmental_Monitoring"},{"id":15836,"name":"Environmental Chemistry","url":"https://www.academia.edu/Documents/in/Environmental_Chemistry"},{"id":26327,"name":"Medicine","url":"https://www.academia.edu/Documents/in/Medicine"},{"id":36763,"name":"Aerosols","url":"https://www.academia.edu/Documents/in/Aerosols"},{"id":43838,"name":"India","url":"https://www.academia.edu/Documents/in/India"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":54259,"name":"Cities","url":"https://www.academia.edu/Documents/in/Cities"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences"},{"id":87501,"name":"Aerosol","url":"https://www.academia.edu/Documents/in/Aerosol"},{"id":260118,"name":"CHEMICAL SCIENCES","url":"https://www.academia.edu/Documents/in/CHEMICAL_SCIENCES"},{"id":283313,"name":"Soot","url":"https://www.academia.edu/Documents/in/Soot"},{"id":649451,"name":"Seasons","url":"https://www.academia.edu/Documents/in/Seasons"},{"id":1297608,"name":"Organic Chemicals","url":"https://www.academia.edu/Documents/in/Organic_Chemicals"},{"id":1656539,"name":"Air Pollutants","url":"https://www.academia.edu/Documents/in/Air_Pollutants"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358527"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/79358527/Analysis_of_the_Variations_of_the_Whitecap_Fraction_as_Measured_in_a_Coastal_Zone"><img alt="Research paper thumbnail of Analysis of the Variations of the Whitecap Fraction as Measured in a Coastal Zone" class="work-thumbnail" src="https://attachments.academia-assets.com/86100496/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/79358527/Analysis_of_the_Variations_of_the_Whitecap_Fraction_as_Measured_in_a_Coastal_Zone">Analysis of the Variations of the Whitecap Fraction as Measured in a Coastal Zone</a></div><div class="wp-workCard_item"><span>Boundary-Layer Meteorology</span><span>, 2004</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The whitecap coverage generated by breaking waves plays a major role in the transfer of heat, mom...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The whitecap coverage generated by breaking waves plays a major role in the transfer of heat, momentum, water vapour and particles at the air-sea interface. The sea surface covered by whitecaps strongly depends on both the wind and the wave-field characteristics. In particular, in coastal zones, the variations of the whitecap fraction, commonly noted W , differ from open ocean conditions, due to fetch effects, wave-current interactions, bottom influence and irregular coastlines affecting both the wind properties and the wave development. We present an analysis of the whitecap-fraction variations using experimental data acquired during FETCH (Flux, Etat de mer, et Télédétection en Condition de fetcH variable), an experimental campaign that took place in the Gulf of Lion off the French Mediterranean coast in 1998. The data include various conditions of wave development associated with fetch and unsteady effects. The whitecap fraction W was measured using an original image processing technique applied to sea surface photography. Specific relationships between the whitecap fraction and both atmospheric and oceanic parameters are investigated, which confirm the suitability of the friction velocity for modelling W. However, W has also been parameterised using wave-parameter dependent relationships, which is of interest for very short fetches.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="92e828c51d5327d0231b4982162d7940" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100496,"asset_id":79358527,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100496/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358527"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358527"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358527; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358527]").text(description); $(".js-view-count[data-work-id=79358527]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358527; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358527']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358527, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "92e828c51d5327d0231b4982162d7940" } } $('.js-work-strip[data-work-id=79358527]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358527,"title":"Analysis of the Variations of the Whitecap Fraction as Measured in a Coastal Zone","translated_title":"","metadata":{"publisher":"Springer Nature","grobid_abstract":"The whitecap coverage generated by breaking waves plays a major role in the transfer of heat, momentum, water vapour and particles at the air-sea interface. The sea surface covered by whitecaps strongly depends on both the wind and the wave-field characteristics. In particular, in coastal zones, the variations of the whitecap fraction, commonly noted W , differ from open ocean conditions, due to fetch effects, wave-current interactions, bottom influence and irregular coastlines affecting both the wind properties and the wave development. We present an analysis of the whitecap-fraction variations using experimental data acquired during FETCH (Flux, Etat de mer, et Télédétection en Condition de fetcH variable), an experimental campaign that took place in the Gulf of Lion off the French Mediterranean coast in 1998. The data include various conditions of wave development associated with fetch and unsteady effects. The whitecap fraction W was measured using an original image processing technique applied to sea surface photography. Specific relationships between the whitecap fraction and both atmospheric and oceanic parameters are investigated, which confirm the suitability of the friction velocity for modelling W. However, W has also been parameterised using wave-parameter dependent relationships, which is of interest for very short fetches.","publication_date":{"day":null,"month":null,"year":2004,"errors":{}},"publication_name":"Boundary-Layer Meteorology","grobid_abstract_attachment_id":86100496},"translated_abstract":null,"internal_url":"https://www.academia.edu/79358527/Analysis_of_the_Variations_of_the_Whitecap_Fraction_as_Measured_in_a_Coastal_Zone","translated_internal_url":"","created_at":"2022-05-18T00:55:19.941-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":40419649,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":86100496,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/86100496/thumbnails/1.jpg","file_name":"Lafon2003_WCCfetch_coastal.pdf","download_url":"https://www.academia.edu/attachments/86100496/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Analysis_of_the_Variations_of_the_Whitec.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/86100496/Lafon2003_WCCfetch_coastal-libre.pdf?1652861541=\u0026response-content-disposition=attachment%3B+filename%3DAnalysis_of_the_Variations_of_the_Whitec.pdf\u0026Expires=1737247635\u0026Signature=dIrw-Rhxkzdjz8T64-reNZdoSVcN2PKRKj31pReygsr7tz0loXaNeJQUUEFSrj9PNpUc4Y0FxaiIIz53x4TbAks7VFc5RsBNB-BWDGZHWLLQGrKKkUYU5Qh6NCuqcAEcZCZ4BO0CUsgXUyw-KJlOMfceVMzymsVssoWWSrl6Sl~nTjGm3OzUwSxx4gO38YW0S7F-NA-qde84hYIjhDFlfq5dGeXNnx-urdgSir4IIDk0vULSjnWuAS-ZPnLyoymzpUTnojToXDPvL5vDPFdVGEYRWvUSoaSlQYXP0gpfrfv1Qa3FeXFIEWTlmixqxtd3w5G-IdhR7ObJurjWet7f6w__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Analysis_of_the_Variations_of_the_Whitecap_Fraction_as_Measured_in_a_Coastal_Zone","translated_slug":"","page_count":22,"language":"en","content_type":"Work","summary":"The whitecap coverage generated by breaking waves plays a major role in the transfer of heat, momentum, water vapour and particles at the air-sea interface. The sea surface covered by whitecaps strongly depends on both the wind and the wave-field characteristics. In particular, in coastal zones, the variations of the whitecap fraction, commonly noted W , differ from open ocean conditions, due to fetch effects, wave-current interactions, bottom influence and irregular coastlines affecting both the wind properties and the wave development. We present an analysis of the whitecap-fraction variations using experimental data acquired during FETCH (Flux, Etat de mer, et Télédétection en Condition de fetcH variable), an experimental campaign that took place in the Gulf of Lion off the French Mediterranean coast in 1998. The data include various conditions of wave development associated with fetch and unsteady effects. The whitecap fraction W was measured using an original image processing technique applied to sea surface photography. Specific relationships between the whitecap fraction and both atmospheric and oceanic parameters are investigated, which confirm the suitability of the friction velocity for modelling W. However, W has also been parameterised using wave-parameter dependent relationships, which is of interest for very short fetches.","owner":{"id":40419649,"first_name":"Jacques","middle_initials":"","last_name":"Piazzola","page_name":"JacquesPiazzola","domain_name":"independent","created_at":"2015-12-20T02:11:32.317-08:00","display_name":"Jacques Piazzola","url":"https://independent.academia.edu/JacquesPiazzola"},"attachments":[{"id":86100496,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/86100496/thumbnails/1.jpg","file_name":"Lafon2003_WCCfetch_coastal.pdf","download_url":"https://www.academia.edu/attachments/86100496/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Analysis_of_the_Variations_of_the_Whitec.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/86100496/Lafon2003_WCCfetch_coastal-libre.pdf?1652861541=\u0026response-content-disposition=attachment%3B+filename%3DAnalysis_of_the_Variations_of_the_Whitec.pdf\u0026Expires=1737247636\u0026Signature=PP7tbG1ewtCnbvTleBgLq4sHTSRF3AwsUnBKbtgq9a-PpqMnDhVEOR0QPy4ceeQGmwbWkcBUvOqf--pQl5IhzQc-nlsjaxSOlQyhzXGnDbzMuXn7EInkj0LYCzzu1647faT5FtXN3UGl~NWFahIX5D~uGwl~6eVWdXIuFxgjI4leMGFV-QvD3tRfyFRHmOgjfuv1Kq6rDl6JKHWAPQR4Uwdu7Gzy7B1GRjaSvqQ4DDZtlWG4GVedU1spLH8fAsql-2cZGMMWvbPsv2T2Y3ZkxcEPz2nnzcG3kRsArL--DRhc~~bEbsVqYkdFmgC2f2YqO5Kf~Rlys2nM0~gnjaLD6Q__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":4062,"name":"Boundary Layer Meteorology","url":"https://www.academia.edu/Documents/in/Boundary_Layer_Meteorology"},{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences"},{"id":116445,"name":"Air-Sea Interaction","url":"https://www.academia.edu/Documents/in/Air-Sea_Interaction"},{"id":477461,"name":"Coastal Zone","url":"https://www.academia.edu/Documents/in/Coastal_Zone"},{"id":500343,"name":"Water vapour","url":"https://www.academia.edu/Documents/in/Water_vapour"},{"id":1120502,"name":"Experimental Data","url":"https://www.academia.edu/Documents/in/Experimental_Data"},{"id":1561715,"name":"Image processing techniques","url":"https://www.academia.edu/Documents/in/Image_processing_techniques"},{"id":4058610,"name":"gulf of lion","url":"https://www.academia.edu/Documents/in/gulf_of_lion"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358519"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/79358519/One_year_measurements_of_aerosol_optical_properties_over_an_urban_coastal_site_Effect_on_local_direct_radiative_forcing"><img alt="Research paper thumbnail of One year measurements of aerosol optical properties over an urban coastal site: Effect on local direct radiative forcing" class="work-thumbnail" src="https://attachments.academia-assets.com/86100481/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/79358519/One_year_measurements_of_aerosol_optical_properties_over_an_urban_coastal_site_Effect_on_local_direct_radiative_forcing">One year measurements of aerosol optical properties over an urban coastal site: Effect on local direct radiative forcing</a></div><div class="wp-workCard_item"><span>Atmospheric Research</span><span>, 2008</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">We present results of direct aerosol radiative forcing over a French Mediterranean coastal zone b...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">We present results of direct aerosol radiative forcing over a French Mediterranean coastal zone based on one year of continuous observations of aerosol optical properties during 2005-2006. Monthly-mean aerosol optical depth at 440 nm ranged between 0.1 and 0.34, with high Angstrom coefficient (α N 1.2). The single scattering albedo (at 525 nm) estimated at the surface ranged between 0.7 and 0.8, indicating significant absorption. The presence of aerosols over the Mediterranean zone during summer decreases the shortwave radiation reaching the surface by as much as 26 ± 3.9 W m − 2 , and increases the top of the atmosphere reflected radiation by as much as 5.2 ± 1.0 W m − 2. The shortwave atmospheric absorption translates to an atmospheric heating of 2.5 to 4.6 K day − 1. Concerted efforts are needed for investigating the possible impact of the increase in heating rate on the maintenance of heatwaves frequently occurring over this coastal region during summer time.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="87b6803be6dd29f477569df36e87f902" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100481,"asset_id":79358519,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100481/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358519"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358519"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358519; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358519]").text(description); $(".js-view-count[data-work-id=79358519]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358519; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358519']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358519, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "87b6803be6dd29f477569df36e87f902" } } $('.js-work-strip[data-work-id=79358519]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358519,"title":"One year measurements of aerosol optical properties over an urban coastal site: Effect on local direct radiative forcing","translated_title":"","metadata":{"publisher":"Elsevier BV","ai_title_tag":"Aerosol Optical Properties and Their Impact on Radiative Forcing","grobid_abstract":"We present results of direct aerosol radiative forcing over a French Mediterranean coastal zone based on one year of continuous observations of aerosol optical properties during 2005-2006. Monthly-mean aerosol optical depth at 440 nm ranged between 0.1 and 0.34, with high Angstrom coefficient (α N 1.2). The single scattering albedo (at 525 nm) estimated at the surface ranged between 0.7 and 0.8, indicating significant absorption. The presence of aerosols over the Mediterranean zone during summer decreases the shortwave radiation reaching the surface by as much as 26 ± 3.9 W m − 2 , and increases the top of the atmosphere reflected radiation by as much as 5.2 ± 1.0 W m − 2. The shortwave atmospheric absorption translates to an atmospheric heating of 2.5 to 4.6 K day − 1. Concerted efforts are needed for investigating the possible impact of the increase in heating rate on the maintenance of heatwaves frequently occurring over this coastal region during summer time.","publication_date":{"day":null,"month":null,"year":2008,"errors":{}},"publication_name":"Atmospheric Research","grobid_abstract_attachment_id":86100481},"translated_abstract":null,"internal_url":"https://www.academia.edu/79358519/One_year_measurements_of_aerosol_optical_properties_over_an_urban_coastal_site_Effect_on_local_direct_radiative_forcing","translated_internal_url":"","created_at":"2022-05-18T00:55:10.857-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":40419649,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":86100481,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/86100481/thumbnails/1.jpg","file_name":"Sahaetal_AtmosRes_2008.pdf","download_url":"https://www.academia.edu/attachments/86100481/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"One_year_measurements_of_aerosol_optical.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/86100481/Sahaetal_AtmosRes_2008-libre.pdf?1652861539=\u0026response-content-disposition=attachment%3B+filename%3DOne_year_measurements_of_aerosol_optical.pdf\u0026Expires=1737247636\u0026Signature=RTQPHgUrg3xMcjRozQ2Qtkk2WUiPl~q5SM-YBG6Br75QCVjcSuBOZ1sdSz1ekpgJknpbwvB1BSd57XvCEQfuLFZrVd-ujLcxx79XluStxxVIkHCxdzMO2aRDeGvt92wsEF1omlSOxsZAmLPGi7MZMFkhcTna3G8nlnRammlNf9ovlqXDzchqbOTUVVU1xvmnR9fmpgLDunBvDYjLB43SOMprkffVH5bnlCwm8zSrHzvdTWkaz3IoNFze9-ern9wZqdeUUlmWSn1kVGiB3CMY2jZKn3SYZg8r2cvlqfTKOAgjuDJxdMpGxDBMeor2mj1qZnrqgTmAUfKG9cznZOUmsQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"One_year_measurements_of_aerosol_optical_properties_over_an_urban_coastal_site_Effect_on_local_direct_radiative_forcing","translated_slug":"","page_count":8,"language":"en","content_type":"Work","summary":"We present results of direct aerosol radiative forcing over a French Mediterranean coastal zone based on one year of continuous observations of aerosol optical properties during 2005-2006. Monthly-mean aerosol optical depth at 440 nm ranged between 0.1 and 0.34, with high Angstrom coefficient (α N 1.2). The single scattering albedo (at 525 nm) estimated at the surface ranged between 0.7 and 0.8, indicating significant absorption. The presence of aerosols over the Mediterranean zone during summer decreases the shortwave radiation reaching the surface by as much as 26 ± 3.9 W m − 2 , and increases the top of the atmosphere reflected radiation by as much as 5.2 ± 1.0 W m − 2. The shortwave atmospheric absorption translates to an atmospheric heating of 2.5 to 4.6 K day − 1. Concerted efforts are needed for investigating the possible impact of the increase in heating rate on the maintenance of heatwaves frequently occurring over this coastal region during summer time.","owner":{"id":40419649,"first_name":"Jacques","middle_initials":"","last_name":"Piazzola","page_name":"JacquesPiazzola","domain_name":"independent","created_at":"2015-12-20T02:11:32.317-08:00","display_name":"Jacques Piazzola","url":"https://independent.academia.edu/JacquesPiazzola"},"attachments":[{"id":86100481,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/86100481/thumbnails/1.jpg","file_name":"Sahaetal_AtmosRes_2008.pdf","download_url":"https://www.academia.edu/attachments/86100481/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"One_year_measurements_of_aerosol_optical.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/86100481/Sahaetal_AtmosRes_2008-libre.pdf?1652861539=\u0026response-content-disposition=attachment%3B+filename%3DOne_year_measurements_of_aerosol_optical.pdf\u0026Expires=1737247636\u0026Signature=RTQPHgUrg3xMcjRozQ2Qtkk2WUiPl~q5SM-YBG6Br75QCVjcSuBOZ1sdSz1ekpgJknpbwvB1BSd57XvCEQfuLFZrVd-ujLcxx79XluStxxVIkHCxdzMO2aRDeGvt92wsEF1omlSOxsZAmLPGi7MZMFkhcTna3G8nlnRammlNf9ovlqXDzchqbOTUVVU1xvmnR9fmpgLDunBvDYjLB43SOMprkffVH5bnlCwm8zSrHzvdTWkaz3IoNFze9-ern9wZqdeUUlmWSn1kVGiB3CMY2jZKn3SYZg8r2cvlqfTKOAgjuDJxdMpGxDBMeor2mj1qZnrqgTmAUfKG9cznZOUmsQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":2442,"name":"Atmospheric Science","url":"https://www.academia.edu/Documents/in/Atmospheric_Science"},{"id":5980,"name":"Atmospheric Modeling","url":"https://www.academia.edu/Documents/in/Atmospheric_Modeling"},{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences"},{"id":185380,"name":"Optical Properties","url":"https://www.academia.edu/Documents/in/Optical_Properties"},{"id":477461,"name":"Coastal Zone","url":"https://www.academia.edu/Documents/in/Coastal_Zone"},{"id":681573,"name":"Heat Wave","url":"https://www.academia.edu/Documents/in/Heat_Wave"},{"id":918758,"name":"Aerosol Optical Depth","url":"https://www.academia.edu/Documents/in/Aerosol_Optical_Depth"},{"id":955957,"name":"Radiative Forcing","url":"https://www.academia.edu/Documents/in/Radiative_Forcing"},{"id":2051052,"name":"Site Effect","url":"https://www.academia.edu/Documents/in/Site_Effect"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358500"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/79358500/Study_of_Vertical_Transport_of_Marine_Aerosol_Using_an_Unsteady_2D_Model"><img alt="Research paper thumbnail of Study of Vertical Transport of Marine Aerosol Using an Unsteady 2D Model" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/79358500/Study_of_Vertical_Transport_of_Marine_Aerosol_Using_an_Unsteady_2D_Model">Study of Vertical Transport of Marine Aerosol Using an Unsteady 2D Model</a></div><div class="wp-workCard_item"><span>NATO Science for Peace and Security Series C: Environmental Security</span><span>, 2011</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358500"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358500"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358500; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358498"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/79358498/Aerosol_concentration_and_fetch"><img alt="Research paper thumbnail of Aerosol concentration and fetch" class="work-thumbnail" src="https://attachments.academia-assets.com/86100463/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/79358498/Aerosol_concentration_and_fetch">Aerosol concentration and fetch</a></div><div class="wp-workCard_item"><span>SPIE Proceedings</span><span>, 1998</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">On the basis of a comprehensive series of measurements on the Irish Atlantic coast, an extension ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">On the basis of a comprehensive series of measurements on the Irish Atlantic coast, an extension of the Navy Aerosol Model (NAM) for the coastal zone is proposed. As in NAM. the dependence of the aerosol concentration on meteorological parameters is parameterized using empirical coefficients. The effect of continental aerosols present in the coastal zone is modeled as a function of fetch. A reasonable agreement is found between the model and the aerosol size distributions as measured on the island Inisheer</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b27c67c6c40a3305677065dbf0f4d149" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100463,"asset_id":79358498,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100463/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358498"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358498"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358498; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358498]").text(description); $(".js-view-count[data-work-id=79358498]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358498; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358498']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358498, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "b27c67c6c40a3305677065dbf0f4d149" } } $('.js-work-strip[data-work-id=79358498]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358498,"title":"Aerosol concentration and fetch","translated_title":"","metadata":{"publisher":"SPIE","grobid_abstract":"On the basis of a comprehensive series of measurements on the Irish Atlantic coast, an extension of the Navy Aerosol Model (NAM) for the coastal zone is proposed. 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The Advanced Navy Aerosol Model (ANAM) aims at providing a quantitative estimate of the aerosol effects on the basis of standard meteorological parameters such as wind speed and relative humidity. For application in coastal regions, the ANAM includes non-marine aerosols that are governed by an ill-defined tuning parameter: the air mass parameter (AMP). The present paper proposes a new parameterization for assessing the effect of these non-marine particles on the propagation. The new parameterization utilizes the Ångström coefficient, which can be experimentally obtained with a sun photometer, and introduces new types of aerosols in ANAM. The new parameterization was tested against experimental validation data acquired at Porquerolles Island at the French Riviera. The limited test data suggested that the new parameterization is only partially efficient in capturing the aerosol signature of the coastal environment. Nevertheless, the new Ångström coefficient algorithm avoids using the ill-defined AMP, and may thus be useful to the ANAM community.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c30b957d8cff29fd91cfd8c4c03517a5" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100464,"asset_id":79358497,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100464/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358497"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358497"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358497; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358497]").text(description); $(".js-view-count[data-work-id=79358497]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358497; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358497']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358497, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "c30b957d8cff29fd91cfd8c4c03517a5" } } $('.js-work-strip[data-work-id=79358497]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358497,"title":"The Advanced Navy Aerosol Model (ANAM): validation of small-particle modes","translated_title":"","metadata":{"publisher":"SPIE","ai_title_tag":"ANAM Validation: New Parameterization for Coastal Aerosols","grobid_abstract":"The image quality of electro-optical sensors in the (lower-altitude marine) atmosphere is limited by aerosols, which cause contrast reduction due to transmission losses and impact on the thermal signature of objects by scattering solar radiation. 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Nevertheless, the new Ångström coefficient algorithm avoids using the ill-defined AMP, and may thus be useful to the ANAM community.","publication_date":{"day":null,"month":null,"year":2011,"errors":{}},"publication_name":"Atmospheric Optics IV: Turbulence and Propagation","grobid_abstract_attachment_id":86100464},"translated_abstract":null,"internal_url":"https://www.academia.edu/79358497/The_Advanced_Navy_Aerosol_Model_ANAM_validation_of_small_particle_modes","translated_internal_url":"","created_at":"2022-05-18T00:54:28.640-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":40419649,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":86100464,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/86100464/thumbnails/1.jpg","file_name":"eijk-2011-advanced.pdf","download_url":"https://www.academia.edu/attachments/86100464/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_Advanced_Navy_Aerosol_Model_ANAM_val.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/86100464/eijk-2011-advanced-libre.pdf?1652861543=\u0026response-content-disposition=attachment%3B+filename%3DThe_Advanced_Navy_Aerosol_Model_ANAM_val.pdf\u0026Expires=1737247636\u0026Signature=gX-s2oJk2bb01dZ0sTiRkImLovA73h1-M0RiLwkfCoREf1uQ6et2Yd7vUW8z3v9lqbu7rsBnpSWpiIuQ6wIo~kejsqIyiyDKBej2-~91Kgf3feLs-NzTixlx8NExnVPlCmkmcekX07PGaSZceO-ZqhDBljXnppQtgAnoos~NBOP~rEPt32SWGiXYY98sf9Lcf8ckM6Lgyr5WH69jgyTRUYPNndzBAVfi-GBpUUkrFCnidQSWtM2EQYwGLj4aLQnZmF2BsQ4Loqw5lbs7NpTbpUsmqt3TiWRgM1IGe9M6HrpzUdL95CzEPIqBrQNs6-LOTNC9cewBx0ev5BAEzw7yag__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_Advanced_Navy_Aerosol_Model_ANAM_validation_of_small_particle_modes","translated_slug":"","page_count":9,"language":"en","content_type":"Work","summary":"The image quality of electro-optical sensors in the (lower-altitude marine) atmosphere is limited by aerosols, which cause contrast reduction due to transmission losses and impact on the thermal signature of objects by scattering solar radiation. The Advanced Navy Aerosol Model (ANAM) aims at providing a quantitative estimate of the aerosol effects on the basis of standard meteorological parameters such as wind speed and relative humidity. For application in coastal regions, the ANAM includes non-marine aerosols that are governed by an ill-defined tuning parameter: the air mass parameter (AMP). The present paper proposes a new parameterization for assessing the effect of these non-marine particles on the propagation. The new parameterization utilizes the Ångström coefficient, which can be experimentally obtained with a sun photometer, and introduces new types of aerosols in ANAM. The new parameterization was tested against experimental validation data acquired at Porquerolles Island at the French Riviera. The limited test data suggested that the new parameterization is only partially efficient in capturing the aerosol signature of the coastal environment. Nevertheless, the new Ångström coefficient algorithm avoids using the ill-defined AMP, and may thus be useful to the ANAM community.","owner":{"id":40419649,"first_name":"Jacques","middle_initials":"","last_name":"Piazzola","page_name":"JacquesPiazzola","domain_name":"independent","created_at":"2015-12-20T02:11:32.317-08:00","display_name":"Jacques Piazzola","url":"https://independent.academia.edu/JacquesPiazzola"},"attachments":[{"id":86100464,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/86100464/thumbnails/1.jpg","file_name":"eijk-2011-advanced.pdf","download_url":"https://www.academia.edu/attachments/86100464/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_Advanced_Navy_Aerosol_Model_ANAM_val.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/86100464/eijk-2011-advanced-libre.pdf?1652861543=\u0026response-content-disposition=attachment%3B+filename%3DThe_Advanced_Navy_Aerosol_Model_ANAM_val.pdf\u0026Expires=1737247636\u0026Signature=gX-s2oJk2bb01dZ0sTiRkImLovA73h1-M0RiLwkfCoREf1uQ6et2Yd7vUW8z3v9lqbu7rsBnpSWpiIuQ6wIo~kejsqIyiyDKBej2-~91Kgf3feLs-NzTixlx8NExnVPlCmkmcekX07PGaSZceO-ZqhDBljXnppQtgAnoos~NBOP~rEPt32SWGiXYY98sf9Lcf8ckM6Lgyr5WH69jgyTRUYPNndzBAVfi-GBpUUkrFCnidQSWtM2EQYwGLj4aLQnZmF2BsQ4Loqw5lbs7NpTbpUsmqt3TiWRgM1IGe9M6HrpzUdL95CzEPIqBrQNs6-LOTNC9cewBx0ev5BAEzw7yag__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":48,"name":"Engineering","url":"https://www.academia.edu/Documents/in/Engineering"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":4758,"name":"Electronics","url":"https://www.academia.edu/Documents/in/Electronics"},{"id":30415,"name":"Image Quality","url":"https://www.academia.edu/Documents/in/Image_Quality"},{"id":120698,"name":"Particles","url":"https://www.academia.edu/Documents/in/Particles"},{"id":230744,"name":"Relative Humidity","url":"https://www.academia.edu/Documents/in/Relative_Humidity"},{"id":284947,"name":"Solar radiation","url":"https://www.academia.edu/Documents/in/Solar_radiation"},{"id":441926,"name":"Scattering","url":"https://www.academia.edu/Documents/in/Scattering"},{"id":444369,"name":"Humidity","url":"https://www.academia.edu/Documents/in/Humidity"},{"id":755542,"name":"Wind Speed","url":"https://www.academia.edu/Documents/in/Wind_Speed"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358496"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/79358496/Aerosol_extinction_in_coastal_zones"><img alt="Research paper thumbnail of Aerosol extinction in coastal zones" class="work-thumbnail" src="https://attachments.academia-assets.com/86100460/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/79358496/Aerosol_extinction_in_coastal_zones">Aerosol extinction in coastal zones</a></div><div class="wp-workCard_item"><span>SPIE Proceedings</span><span>, 2004</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The performance of electro-optical systems can be substantially affected by aerosol particles tha...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The performance of electro-optical systems can be substantially affected by aerosol particles that scatter and absorb electromagnetic radiation. A few years ago, an empirical model was developed describing the aerosol size distributions in the Mediterranean coastal atmosphere near Toulon (France). This model has been coupled with Mie theory to yield the code MEDEX (MEDiterranean EXtinction) for the aerosol extinction. This contribution deals with the evaluation of MEDEX for aerosol data recorded near the Black Sea coast. For this site, MEDEX correctly predicts the aerosol extinction as function of wavelength, albeit with minor discrepancies below one micron. These differences are attributed to the uncertainty in predicting the concentrations of submicron particles. The comparison shows that MEDEX may be more generally applicable than to the Toulon area.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e955d61ed1a591f1e68b4cab71c7e29f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100460,"asset_id":79358496,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100460/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358496"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358496"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358496; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358496]").text(description); $(".js-view-count[data-work-id=79358496]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358496; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358496']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358496, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "e955d61ed1a591f1e68b4cab71c7e29f" } } $('.js-work-strip[data-work-id=79358496]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358496,"title":"Aerosol extinction in coastal zones","translated_title":"","metadata":{"publisher":"SPIE","grobid_abstract":"The performance of electro-optical systems can be substantially affected by aerosol particles that scatter and absorb electromagnetic radiation. A few years ago, an empirical model was developed describing the aerosol size distributions in the Mediterranean coastal atmosphere near Toulon (France). This model has been coupled with Mie theory to yield the code MEDEX (MEDiterranean EXtinction) for the aerosol extinction. This contribution deals with the evaluation of MEDEX for aerosol data recorded near the Black Sea coast. For this site, MEDEX correctly predicts the aerosol extinction as function of wavelength, albeit with minor discrepancies below one micron. These differences are attributed to the uncertainty in predicting the concentrations of submicron particles. The comparison shows that MEDEX may be more generally applicable than to the Toulon area.","publication_date":{"day":null,"month":null,"year":2004,"errors":{}},"publication_name":"SPIE Proceedings","grobid_abstract_attachment_id":86100460},"translated_abstract":null,"internal_url":"https://www.academia.edu/79358496/Aerosol_extinction_in_coastal_zones","translated_internal_url":"","created_at":"2022-05-18T00:54:28.541-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":40419649,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":86100460,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/86100460/thumbnails/1.jpg","file_name":"piazzola-2004-aerosol.pdf","download_url":"https://www.academia.edu/attachments/86100460/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Aerosol_extinction_in_coastal_zones.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/86100460/piazzola-2004-aerosol-libre.pdf?1652861543=\u0026response-content-disposition=attachment%3B+filename%3DAerosol_extinction_in_coastal_zones.pdf\u0026Expires=1737247636\u0026Signature=dipJMgb6sqMWS3pvEqpu0z9qxvahxawFTQOgMg2119rd~Xt23HUKdvvTXoC~6jf6p1yJqhuFnPn~c~RLLqPYNcU7B5k84HDzd1nJk1hq2vwH49UXmEn6owGrDoXEwzC1usVaZL5lnRoyr0IW~8VvzjZYxGInab1BCN4iV0YWXaAJMGct65IFPUtSuqs6XHzBlASVsBostjPuHrGdhkLbBs6HL33ADp1tz72VxvTi00ixoWzyAZfdYOq44FxhggFOaBt-Bxruj8aIY4XV9oMzwwDwJzToSPpQTCm5Y-T1gRmb6evqXgLLHuN1sZEqgDBBN7aMRG~oM26JWOUZsBotIA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Aerosol_extinction_in_coastal_zones","translated_slug":"","page_count":7,"language":"en","content_type":"Work","summary":"The performance of electro-optical systems can be substantially affected by aerosol particles that scatter and absorb electromagnetic radiation. A few years ago, an empirical model was developed describing the aerosol size distributions in the Mediterranean coastal atmosphere near Toulon (France). This model has been coupled with Mie theory to yield the code MEDEX (MEDiterranean EXtinction) for the aerosol extinction. This contribution deals with the evaluation of MEDEX for aerosol data recorded near the Black Sea coast. For this site, MEDEX correctly predicts the aerosol extinction as function of wavelength, albeit with minor discrepancies below one micron. These differences are attributed to the uncertainty in predicting the concentrations of submicron particles. The comparison shows that MEDEX may be more generally applicable than to the Toulon area.","owner":{"id":40419649,"first_name":"Jacques","middle_initials":"","last_name":"Piazzola","page_name":"JacquesPiazzola","domain_name":"independent","created_at":"2015-12-20T02:11:32.317-08:00","display_name":"Jacques Piazzola","url":"https://independent.academia.edu/JacquesPiazzola"},"attachments":[{"id":86100460,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/86100460/thumbnails/1.jpg","file_name":"piazzola-2004-aerosol.pdf","download_url":"https://www.academia.edu/attachments/86100460/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Aerosol_extinction_in_coastal_zones.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/86100460/piazzola-2004-aerosol-libre.pdf?1652861543=\u0026response-content-disposition=attachment%3B+filename%3DAerosol_extinction_in_coastal_zones.pdf\u0026Expires=1737247636\u0026Signature=dipJMgb6sqMWS3pvEqpu0z9qxvahxawFTQOgMg2119rd~Xt23HUKdvvTXoC~6jf6p1yJqhuFnPn~c~RLLqPYNcU7B5k84HDzd1nJk1hq2vwH49UXmEn6owGrDoXEwzC1usVaZL5lnRoyr0IW~8VvzjZYxGInab1BCN4iV0YWXaAJMGct65IFPUtSuqs6XHzBlASVsBostjPuHrGdhkLbBs6HL33ADp1tz72VxvTi00ixoWzyAZfdYOq44FxhggFOaBt-Bxruj8aIY4XV9oMzwwDwJzToSPpQTCm5Y-T1gRmb6evqXgLLHuN1sZEqgDBBN7aMRG~oM26JWOUZsBotIA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":1252,"name":"Remote Sensing","url":"https://www.academia.edu/Documents/in/Remote_Sensing"},{"id":73142,"name":"Electromagnetic Radiation","url":"https://www.academia.edu/Documents/in/Electromagnetic_Radiation"},{"id":87501,"name":"Aerosol","url":"https://www.academia.edu/Documents/in/Aerosol"},{"id":477461,"name":"Coastal Zone","url":"https://www.academia.edu/Documents/in/Coastal_Zone"},{"id":877520,"name":"Electro-optic modulators","url":"https://www.academia.edu/Documents/in/Electro-optic_modulators"},{"id":1297237,"name":"Empirical Model","url":"https://www.academia.edu/Documents/in/Empirical_Model"}],"urls":[{"id":20551563,"url":"http://proceedings.spiedigitallibrary.org/proceeding.aspx?doi=10.1117/12.563299"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358495"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/79358495/Extension_of_the_Navy_aerosol_model_to_coastal_areas"><img alt="Research paper thumbnail of Extension of the Navy aerosol model to coastal areas" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/79358495/Extension_of_the_Navy_aerosol_model_to_coastal_areas">Extension of the Navy aerosol model to coastal areas</a></div><div class="wp-workCard_item"><span>Optical Engineering</span><span>, 2000</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The performance assessment of electro-optical systems with propagation prediction codes requires ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The performance assessment of electro-optical systems with propagation prediction codes requires accurate atmospheric models. The model that is most frequently used for the prediction of aerosols and their effect on extinction in the marine atmosphere is the U.S. Navy aerosol model (NAM) (Gathman, 1983). The NAM was developed for open ocean applications, where it works well. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358494"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/79358494/Marine_aerosol_concentrations_at_different_locations_of_the_northern_hemisphere"><img alt="Research paper thumbnail of Marine aerosol concentrations at different locations of the northern hemisphere" class="work-thumbnail" src="https://attachments.academia-assets.com/86100461/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/79358494/Marine_aerosol_concentrations_at_different_locations_of_the_northern_hemisphere">Marine aerosol concentrations at different locations of the northern hemisphere</a></div><div class="wp-workCard_item"><span>Journal of Aerosol Science</span><span>, 1998</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a453e44925819533dc7f6c62a5e03fb5" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100461,"asset_id":79358494,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100461/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358494"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358494"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358494; 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href="https://www.academia.edu/93272081/Les_%C3%AEles_d_Hy%C3%A8res_dans_le_syst%C3%A8me_de_circulation_marine_et_atmosph%C3%A9rique_de_la_M%C3%A9diterran%C3%A9e"><img alt="Research paper thumbnail of Les îles d’Hyères dans le système de circulation marine et atmosphérique de la Méditerranée" class="work-thumbnail" src="https://attachments.academia-assets.com/96055012/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/93272081/Les_%C3%AEles_d_Hy%C3%A8res_dans_le_syst%C3%A8me_de_circulation_marine_et_atmosph%C3%A9rique_de_la_M%C3%A9diterran%C3%A9e">Les îles d’Hyères dans le système de circulation marine et atmosphérique de la Méditerranée</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Cet article a pour but de présenter les grandes lignes du 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class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/93272080/Development_of_a_sea_salt_emission_parameterization_for_the_North_western_Mediterranean"><img alt="Research paper thumbnail of Development of a sea salt emission parameterization for the North-western Mediterranean" class="work-thumbnail" src="https://attachments.academia-assets.com/96055008/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/93272080/Development_of_a_sea_salt_emission_parameterization_for_the_North_western_Mediterranean">Development of a sea salt emission parameterization for the North-western Mediterranean</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The aim of the present work is to determinate an accurate formulation for the sea-spray source fu...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The aim of the present work is to determinate an accurate formulation for the sea-spray source function issued from the bubble bursting processes. To this end, a simple aerosol transport Model, the Macmod Model (Tedeschi and Piazzola, 2011) was implemented in the Mediterranean area using different flux formulations for the sea spray source function (e.g., Demoisson et al., 2013; Gong et al., 2003; Monahan et al., 1986; Odvanevaite et al., 2014). The simulations were then compared to a large data set dealing with the aerosol size distributions acquired during an extensive series of measurements in the Northwestern Mediterranean. The results, which are part of an article that will be submitted soon, allowed determination of an accurate sea-spray source function formulation and its dependence on the wave development.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d1aa795168a8acd2cd2fed845e0ada2b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":96055008,"asset_id":93272080,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/96055008/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&st=MTczNzI0NDAzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="93272080"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="93272080"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 93272080; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=93272080]").text(description); $(".js-view-count[data-work-id=93272080]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 93272080; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='93272080']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 93272080, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "d1aa795168a8acd2cd2fed845e0ada2b" } } $('.js-work-strip[data-work-id=93272080]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":93272080,"title":"Development of a sea salt emission parameterization for the North-western Mediterranean","translated_title":"","metadata":{"abstract":"The aim of the present work is to determinate an accurate formulation for the sea-spray source function issued from the bubble bursting processes. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358690"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/79358690/Study_of_the_Impact_of_the_Natural_Production_of_Coastal_Marine_Aerosols_on_the_Dynamics_and_Microphysical_Behavior_of_a_Convective_Cloud"><img alt="Research paper thumbnail of Study of the Impact of the Natural Production of Coastal Marine Aerosols on the Dynamics and Microphysical Behavior of a Convective Cloud" class="work-thumbnail" src="https://attachments.academia-assets.com/86100613/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/79358690/Study_of_the_Impact_of_the_Natural_Production_of_Coastal_Marine_Aerosols_on_the_Dynamics_and_Microphysical_Behavior_of_a_Convective_Cloud">Study of the Impact of the Natural Production of Coastal Marine Aerosols on the Dynamics and Microphysical Behavior of a Convective Cloud</a></div><div class="wp-workCard_item"><span>IEEE Geoscience and Remote Sensing Letters</span><span>, 2013</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The atmosphere contains suspended particles of various origins natural or anthropogenic that cons...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The atmosphere contains suspended particles of various origins natural or anthropogenic that constitutes the atmospheric aerosol. The aerosol cloud interaction is a fundamental mechanis m that influences the precipitation process. To study the impact of ma rine aerosols, especially those generated in coastal areas, on the dynamics and microphysical behavior of the clouds, two numerical models were coupled. The first, calculates the coastal ma rine aerosol spectrum that could be generated under a given weather condition at the sea surface. The p redicted spectrum is then introduced, as in itial aerosol spectra, to a cloud model with a detailed microphysics. The simulat ions performed have focused on a convective cloud (mixed phase) using distinct initial aerosols spectra of different origins in order to highlight the potential effect of ma rine aerosol naturally produced in surf zone on the dynamics and microphysics of the cloud. The results carried out indicates an important contribution of marine aerosol in the process of precipitation formation by promoting an early start of precipitat ion at lower alt itudes, leading to increased amounts of precipitation reaching the ground.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="bd1d964b1f01880521feb663b998e43b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100613,"asset_id":79358690,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100613/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&st=MTczNzI0NDAzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358690"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358690"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358690; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358690]").text(description); $(".js-view-count[data-work-id=79358690]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358690; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358690']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358690, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "bd1d964b1f01880521feb663b998e43b" } } $('.js-work-strip[data-work-id=79358690]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358690,"title":"Study of the Impact of the Natural Production of Coastal Marine Aerosols on the Dynamics and Microphysical Behavior of a Convective Cloud","translated_title":"","metadata":{"publisher":"Institute of Electrical and Electronics Engineers","grobid_abstract":"The atmosphere contains suspended particles of various origins natural or anthropogenic that constitutes the atmospheric aerosol. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358623"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/79358623/Sea_spray_aerosols_and_SARS_Cov_2_an_analysis_using_AERONET_data"><img alt="Research paper thumbnail of Sea-spray aerosols and SARS-Cov-2: an analysis using AERONET data" class="work-thumbnail" src="https://attachments.academia-assets.com/86100558/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/79358623/Sea_spray_aerosols_and_SARS_Cov_2_an_analysis_using_AERONET_data">Sea-spray aerosols and SARS-Cov-2: an analysis using AERONET data</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Even if the people density, habits and displacements probably represent the most important causes...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Even if the people density, habits and displacements probably represent the most important causes of the SARS-Cov-2 virus propagation, the role of the atmospheric aerosol in COVID-19 outbreaks is significant and it needs to be further investigated. Therefore, we aimed to study if the aerosol properties related to the different sources and meteorological conditions we can observe in continental and coastal urbanized areas can have an influence on the atmospheric transport of the SARS-Cov-2 virus. This paper focuses on the lockdown period to reduce the differences in the social behavior. As an example, we investigated the contamination cases during March 2020 in two specific French areas located in both continental and coastal areas with regard to the meteorological conditions and the corresponding aerosol properties. To this end, we used both the optical depth (AOD) and the Angstrom exponent provided by the AERONET network. The results show that the analysis of aerosol ground-based d...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="409eeed45e9fbdc1e1dd09affa93592f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100558,"asset_id":79358623,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100558/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&st=MTczNzI0NDAzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358623"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358623"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358623; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358623]").text(description); $(".js-view-count[data-work-id=79358623]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358623; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358623']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358623, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "409eeed45e9fbdc1e1dd09affa93592f" } } $('.js-work-strip[data-work-id=79358623]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358623,"title":"Sea-spray aerosols and SARS-Cov-2: an analysis using AERONET data","translated_title":"","metadata":{"abstract":"Even if the people density, habits and displacements probably represent the most important causes of the SARS-Cov-2 virus propagation, the role of the atmospheric aerosol in COVID-19 outbreaks is significant and it needs to be further investigated. 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The model that is most frequently used for the prediction of aerosols and their effect on extinction in the marine atmosphere is the US Navy Aerosol Model (NAM). However, NAM can be significantly less reliable in coastal areas than on the open ocean. Based on an extensive series of measurements conducted on the island of Inisheer (Irish West Coast), an empirical aerosol model for the coastal zone formulated as an extension of NAM, in which coastal effects are modeled as a function of fetch, has been developed. This work is extended to the Mediterranean using an aerosol dataset recorded on the island of Porquerolles in the Bay of Toulon (France) and has been coupled with the Mie theory to give a code for the extinction, the code MEDiterranean EXtinction (MEDEX).</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2e666c0e715c1953a002d848d01dfe24" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100535,"asset_id":79358592,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100535/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&st=MTczNzI0NDAzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358592"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358592"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358592; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358592]").text(description); $(".js-view-count[data-work-id=79358592]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358592; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358592']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358592, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "2e666c0e715c1953a002d848d01dfe24" } } $('.js-work-strip[data-work-id=79358592]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358592,"title":"Development of the Mediterranean extinction code (MEDEX)","translated_title":"","metadata":{"publisher":"SPIE-Intl Soc Optical Eng","grobid_abstract":"The performance of electro-optical systems can be substantially affected by aerosol particles that scatter and absorb electromagnetic radiation. The model that is most frequently used for the prediction of aerosols and their effect on extinction in the marine atmosphere is the US Navy Aerosol Model (NAM). However, NAM can be significantly less reliable in coastal areas than on the open ocean. Based on an extensive series of measurements conducted on the island of Inisheer (Irish West Coast), an empirical aerosol model for the coastal zone formulated as an extension of NAM, in which coastal effects are modeled as a function of fetch, has been developed. 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The model that is most frequently used for the prediction of aerosols and their effect on extinction in the marine atmosphere is the US Navy Aerosol Model (NAM). However, NAM can be significantly less reliable in coastal areas than on the open ocean. Based on an extensive series of measurements conducted on the island of Inisheer (Irish West Coast), an empirical aerosol model for the coastal zone formulated as an extension of NAM, in which coastal effects are modeled as a function of fetch, has been developed. 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In particular, it is well recognized that the whitecap cover induced by breaking waves allows substantial enhancement of heat, momentum, gas and particle transfer at the air-sea interface. A large number of studies were conducted during the last decades on the variation of the whitecap fraction, commonly noted W. The results presented in this paper deal with the evolution of the whitecap coverage in coastal zone. In such areas, the wave field is often unsteady with an important variety of sea state developments. The present analysis is based on an extensive series of data obtained during an experimental campaign which took place on the Mediterranean coast in 2001. The results allow observation of the influence of the sea state conditions of the wave field on the whitecap coverage. In addition, this paper confirms the occurrence of a peak in the variations of the whitecap fraction with the wave age for coastal areas as suggested by Lafon et al. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358542"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/79358542/Variations_of_the_aerosol_concentration_with_fetch"><img alt="Research paper thumbnail of Variations of the aerosol concentration with fetch" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/79358542/Variations_of_the_aerosol_concentration_with_fetch">Variations of the aerosol concentration with fetch</a></div><div class="wp-workCard_item"><span>Journal of Aerosol Science</span><span>, 1999</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358542"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358542"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358542; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358542]").text(description); $(".js-view-count[data-work-id=79358542]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358542; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358542']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358542, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=79358542]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358542,"title":"Variations of the aerosol concentration with fetch","translated_title":"","metadata":{"publisher":"Elsevier BV","publication_date":{"day":null,"month":null,"year":1999,"errors":{}},"publication_name":"Journal of Aerosol Science"},"translated_abstract":null,"internal_url":"https://www.academia.edu/79358542/Variations_of_the_aerosol_concentration_with_fetch","translated_internal_url":"","created_at":"2022-05-18T00:55:46.879-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":40419649,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Variations_of_the_aerosol_concentration_with_fetch","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":null,"owner":{"id":40419649,"first_name":"Jacques","middle_initials":"","last_name":"Piazzola","page_name":"JacquesPiazzola","domain_name":"independent","created_at":"2015-12-20T02:11:32.317-08:00","display_name":"Jacques Piazzola","url":"https://independent.academia.edu/JacquesPiazzola"},"attachments":[],"research_interests":[{"id":72,"name":"Chemical Engineering","url":"https://www.academia.edu/Documents/in/Chemical_Engineering"},{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences"},{"id":1759667,"name":"Aerosol Science","url":"https://www.academia.edu/Documents/in/Aerosol_Science"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358540"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/79358540/Characterization_of_carbonaceous_aerosols_over_Delhi_in_Ganga_basin_seasonal_variability_and_possible_sources"><img alt="Research paper thumbnail of Characterization of carbonaceous aerosols over Delhi in Ganga basin: seasonal variability and possible sources" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/79358540/Characterization_of_carbonaceous_aerosols_over_Delhi_in_Ganga_basin_seasonal_variability_and_possible_sources">Characterization of carbonaceous aerosols over Delhi in Ganga basin: seasonal variability and possible sources</a></div><div class="wp-workCard_item"><span>Environmental Science and Pollution Research</span><span>, 2014</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The mass concentration of carbonaceous species, organic carbon (OC), and elemental carbon (EC) us...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The mass concentration of carbonaceous species, organic carbon (OC), and elemental carbon (EC) using a semicontinuous thermo-optical EC-OC analyzer, and black carbon (BC) using an Aethalometer were measured simultaneously at an urban mega city Delhi in Ganga basin from January 2011 to May 2012. The concentrations of OC, EC, and BC exhibit seasonal variability, and their concentrations were ∼2 times higher during winter (OC 38.1 ± 17.9 μg m(-3), EC 15.8 ± 7.3 μg m(-3), and BC 10.1 ± 5.3 μg m(-3)) compared to those in summer (OC 14.1 ± 4.3 μg m(-3), EC 7.5 ± 1.5 μg m(-3), and BC 4.9 ± 1.5 μg m(-3)). A significant correlation between OC and EC (R = 0.95, n = 232) indicate their common emission sources with relatively lower OC/EC ratio (range 1.0-3.6, mean 2.2 ± 0.5) suggests fossil fuel emission as a major source of carbonaceous aerosols over the station. On average, mass concentration of EC was found to be ∼38 % higher than BC during the study period. The measured absorption coefficient (babs) was significantly correlated with EC, suggesting EC as a major absorbing species in ambient aerosols at Delhi. Furthermore, the estimated mass absorption efficiency (σabs) values are similar during winter (5.0 ± 1.5 m(2) g(-1)) and summer (4.8 ± 2.8 m(2) g(-1)). Significantly high aerosol loading of carbonaceous species emphasize an urgent need to focus on air quality management and proper impact assessment on health perspective in these regions.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358540"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358540"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358540; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358540]").text(description); $(".js-view-count[data-work-id=79358540]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358540; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358540']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358540, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=79358540]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358540,"title":"Characterization of carbonaceous aerosols over Delhi in Ganga basin: seasonal variability and possible sources","translated_title":"","metadata":{"abstract":"The mass concentration of carbonaceous species, organic carbon (OC), and elemental carbon (EC) using a semicontinuous thermo-optical EC-OC analyzer, and black carbon (BC) using an Aethalometer were measured simultaneously at an urban mega city Delhi in Ganga basin from January 2011 to May 2012. The concentrations of OC, EC, and BC exhibit seasonal variability, and their concentrations were ∼2 times higher during winter (OC 38.1 ± 17.9 μg m(-3), EC 15.8 ± 7.3 μg m(-3), and BC 10.1 ± 5.3 μg m(-3)) compared to those in summer (OC 14.1 ± 4.3 μg m(-3), EC 7.5 ± 1.5 μg m(-3), and BC 4.9 ± 1.5 μg m(-3)). A significant correlation between OC and EC (R = 0.95, n = 232) indicate their common emission sources with relatively lower OC/EC ratio (range 1.0-3.6, mean 2.2 ± 0.5) suggests fossil fuel emission as a major source of carbonaceous aerosols over the station. On average, mass concentration of EC was found to be ∼38 % higher than BC during the study period. The measured absorption coefficient (babs) was significantly correlated with EC, suggesting EC as a major absorbing species in ambient aerosols at Delhi. Furthermore, the estimated mass absorption efficiency (σabs) values are similar during winter (5.0 ± 1.5 m(2) g(-1)) and summer (4.8 ± 2.8 m(2) g(-1)). Significantly high aerosol loading of carbonaceous species emphasize an urgent need to focus on air quality management and proper impact assessment on health perspective in these regions.","publisher":"Springer Nature","publication_date":{"day":null,"month":null,"year":2014,"errors":{}},"publication_name":"Environmental Science and Pollution Research"},"translated_abstract":"The mass concentration of carbonaceous species, organic carbon (OC), and elemental carbon (EC) using a semicontinuous thermo-optical EC-OC analyzer, and black carbon (BC) using an Aethalometer were measured simultaneously at an urban mega city Delhi in Ganga basin from January 2011 to May 2012. The concentrations of OC, EC, and BC exhibit seasonal variability, and their concentrations were ∼2 times higher during winter (OC 38.1 ± 17.9 μg m(-3), EC 15.8 ± 7.3 μg m(-3), and BC 10.1 ± 5.3 μg m(-3)) compared to those in summer (OC 14.1 ± 4.3 μg m(-3), EC 7.5 ± 1.5 μg m(-3), and BC 4.9 ± 1.5 μg m(-3)). A significant correlation between OC and EC (R = 0.95, n = 232) indicate their common emission sources with relatively lower OC/EC ratio (range 1.0-3.6, mean 2.2 ± 0.5) suggests fossil fuel emission as a major source of carbonaceous aerosols over the station. On average, mass concentration of EC was found to be ∼38 % higher than BC during the study period. The measured absorption coefficient (babs) was significantly correlated with EC, suggesting EC as a major absorbing species in ambient aerosols at Delhi. Furthermore, the estimated mass absorption efficiency (σabs) values are similar during winter (5.0 ± 1.5 m(2) g(-1)) and summer (4.8 ± 2.8 m(2) g(-1)). Significantly high aerosol loading of carbonaceous species emphasize an urgent need to focus on air quality management and proper impact assessment on health perspective in these regions.","internal_url":"https://www.academia.edu/79358540/Characterization_of_carbonaceous_aerosols_over_Delhi_in_Ganga_basin_seasonal_variability_and_possible_sources","translated_internal_url":"","created_at":"2022-05-18T00:55:36.806-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":40419649,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Characterization_of_carbonaceous_aerosols_over_Delhi_in_Ganga_basin_seasonal_variability_and_possible_sources","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"The mass concentration of carbonaceous species, organic carbon (OC), and elemental carbon (EC) using a semicontinuous thermo-optical EC-OC analyzer, and black carbon (BC) using an Aethalometer were measured simultaneously at an urban mega city Delhi in Ganga basin from January 2011 to May 2012. The concentrations of OC, EC, and BC exhibit seasonal variability, and their concentrations were ∼2 times higher during winter (OC 38.1 ± 17.9 μg m(-3), EC 15.8 ± 7.3 μg m(-3), and BC 10.1 ± 5.3 μg m(-3)) compared to those in summer (OC 14.1 ± 4.3 μg m(-3), EC 7.5 ± 1.5 μg m(-3), and BC 4.9 ± 1.5 μg m(-3)). A significant correlation between OC and EC (R = 0.95, n = 232) indicate their common emission sources with relatively lower OC/EC ratio (range 1.0-3.6, mean 2.2 ± 0.5) suggests fossil fuel emission as a major source of carbonaceous aerosols over the station. On average, mass concentration of EC was found to be ∼38 % higher than BC during the study period. The measured absorption coefficient (babs) was significantly correlated with EC, suggesting EC as a major absorbing species in ambient aerosols at Delhi. Furthermore, the estimated mass absorption efficiency (σabs) values are similar during winter (5.0 ± 1.5 m(2) g(-1)) and summer (4.8 ± 2.8 m(2) g(-1)). Significantly high aerosol loading of carbonaceous species emphasize an urgent need to focus on air quality management and proper impact assessment on health perspective in these regions.","owner":{"id":40419649,"first_name":"Jacques","middle_initials":"","last_name":"Piazzola","page_name":"JacquesPiazzola","domain_name":"independent","created_at":"2015-12-20T02:11:32.317-08:00","display_name":"Jacques Piazzola","url":"https://independent.academia.edu/JacquesPiazzola"},"attachments":[],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":523,"name":"Chemistry","url":"https://www.academia.edu/Documents/in/Chemistry"},{"id":5303,"name":"Carbon","url":"https://www.academia.edu/Documents/in/Carbon"},{"id":11801,"name":"Environmental Monitoring","url":"https://www.academia.edu/Documents/in/Environmental_Monitoring"},{"id":15836,"name":"Environmental Chemistry","url":"https://www.academia.edu/Documents/in/Environmental_Chemistry"},{"id":26327,"name":"Medicine","url":"https://www.academia.edu/Documents/in/Medicine"},{"id":36763,"name":"Aerosols","url":"https://www.academia.edu/Documents/in/Aerosols"},{"id":43838,"name":"India","url":"https://www.academia.edu/Documents/in/India"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":54259,"name":"Cities","url":"https://www.academia.edu/Documents/in/Cities"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences"},{"id":87501,"name":"Aerosol","url":"https://www.academia.edu/Documents/in/Aerosol"},{"id":260118,"name":"CHEMICAL SCIENCES","url":"https://www.academia.edu/Documents/in/CHEMICAL_SCIENCES"},{"id":283313,"name":"Soot","url":"https://www.academia.edu/Documents/in/Soot"},{"id":649451,"name":"Seasons","url":"https://www.academia.edu/Documents/in/Seasons"},{"id":1297608,"name":"Organic Chemicals","url":"https://www.academia.edu/Documents/in/Organic_Chemicals"},{"id":1656539,"name":"Air Pollutants","url":"https://www.academia.edu/Documents/in/Air_Pollutants"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358527"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/79358527/Analysis_of_the_Variations_of_the_Whitecap_Fraction_as_Measured_in_a_Coastal_Zone"><img alt="Research paper thumbnail of Analysis of the Variations of the Whitecap Fraction as Measured in a Coastal Zone" class="work-thumbnail" src="https://attachments.academia-assets.com/86100496/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/79358527/Analysis_of_the_Variations_of_the_Whitecap_Fraction_as_Measured_in_a_Coastal_Zone">Analysis of the Variations of the Whitecap Fraction as Measured in a Coastal Zone</a></div><div class="wp-workCard_item"><span>Boundary-Layer Meteorology</span><span>, 2004</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The whitecap coverage generated by breaking waves plays a major role in the transfer of heat, mom...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The whitecap coverage generated by breaking waves plays a major role in the transfer of heat, momentum, water vapour and particles at the air-sea interface. The sea surface covered by whitecaps strongly depends on both the wind and the wave-field characteristics. In particular, in coastal zones, the variations of the whitecap fraction, commonly noted W , differ from open ocean conditions, due to fetch effects, wave-current interactions, bottom influence and irregular coastlines affecting both the wind properties and the wave development. We present an analysis of the whitecap-fraction variations using experimental data acquired during FETCH (Flux, Etat de mer, et Télédétection en Condition de fetcH variable), an experimental campaign that took place in the Gulf of Lion off the French Mediterranean coast in 1998. The data include various conditions of wave development associated with fetch and unsteady effects. The whitecap fraction W was measured using an original image processing technique applied to sea surface photography. Specific relationships between the whitecap fraction and both atmospheric and oceanic parameters are investigated, which confirm the suitability of the friction velocity for modelling W. However, W has also been parameterised using wave-parameter dependent relationships, which is of interest for very short fetches.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="92e828c51d5327d0231b4982162d7940" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100496,"asset_id":79358527,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100496/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358527"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358527"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358527; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358527]").text(description); $(".js-view-count[data-work-id=79358527]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358527; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358527']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358527, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "92e828c51d5327d0231b4982162d7940" } } $('.js-work-strip[data-work-id=79358527]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358527,"title":"Analysis of the Variations of the Whitecap Fraction as Measured in a Coastal Zone","translated_title":"","metadata":{"publisher":"Springer Nature","grobid_abstract":"The whitecap coverage generated by breaking waves plays a major role in the transfer of heat, momentum, water vapour and particles at the air-sea interface. 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Monthly-mean aerosol optical depth at 440 nm ranged between 0.1 and 0.34, with high Angstrom coefficient (α N 1.2). The single scattering albedo (at 525 nm) estimated at the surface ranged between 0.7 and 0.8, indicating significant absorption. The presence of aerosols over the Mediterranean zone during summer decreases the shortwave radiation reaching the surface by as much as 26 ± 3.9 W m − 2 , and increases the top of the atmosphere reflected radiation by as much as 5.2 ± 1.0 W m − 2. The shortwave atmospheric absorption translates to an atmospheric heating of 2.5 to 4.6 K day − 1. Concerted efforts are needed for investigating the possible impact of the increase in heating rate on the maintenance of heatwaves frequently occurring over this coastal region during summer time.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="87b6803be6dd29f477569df36e87f902" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100481,"asset_id":79358519,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100481/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358519"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358519"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358519; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358519]").text(description); $(".js-view-count[data-work-id=79358519]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358519; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358519']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358519, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "87b6803be6dd29f477569df36e87f902" } } $('.js-work-strip[data-work-id=79358519]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358519,"title":"One year measurements of aerosol optical properties over an urban coastal site: Effect on local direct radiative forcing","translated_title":"","metadata":{"publisher":"Elsevier BV","ai_title_tag":"Aerosol Optical Properties and Their Impact on Radiative Forcing","grobid_abstract":"We present results of direct aerosol radiative forcing over a French Mediterranean coastal zone based on one year of continuous observations of aerosol optical properties during 2005-2006. Monthly-mean aerosol optical depth at 440 nm ranged between 0.1 and 0.34, with high Angstrom coefficient (α N 1.2). The single scattering albedo (at 525 nm) estimated at the surface ranged between 0.7 and 0.8, indicating significant absorption. The presence of aerosols over the Mediterranean zone during summer decreases the shortwave radiation reaching the surface by as much as 26 ± 3.9 W m − 2 , and increases the top of the atmosphere reflected radiation by as much as 5.2 ± 1.0 W m − 2. The shortwave atmospheric absorption translates to an atmospheric heating of 2.5 to 4.6 K day − 1. Concerted efforts are needed for investigating the possible impact of the increase in heating rate on the maintenance of heatwaves frequently occurring over this coastal region during summer time.","publication_date":{"day":null,"month":null,"year":2008,"errors":{}},"publication_name":"Atmospheric Research","grobid_abstract_attachment_id":86100481},"translated_abstract":null,"internal_url":"https://www.academia.edu/79358519/One_year_measurements_of_aerosol_optical_properties_over_an_urban_coastal_site_Effect_on_local_direct_radiative_forcing","translated_internal_url":"","created_at":"2022-05-18T00:55:10.857-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":40419649,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":86100481,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/86100481/thumbnails/1.jpg","file_name":"Sahaetal_AtmosRes_2008.pdf","download_url":"https://www.academia.edu/attachments/86100481/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"One_year_measurements_of_aerosol_optical.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/86100481/Sahaetal_AtmosRes_2008-libre.pdf?1652861539=\u0026response-content-disposition=attachment%3B+filename%3DOne_year_measurements_of_aerosol_optical.pdf\u0026Expires=1737247636\u0026Signature=RTQPHgUrg3xMcjRozQ2Qtkk2WUiPl~q5SM-YBG6Br75QCVjcSuBOZ1sdSz1ekpgJknpbwvB1BSd57XvCEQfuLFZrVd-ujLcxx79XluStxxVIkHCxdzMO2aRDeGvt92wsEF1omlSOxsZAmLPGi7MZMFkhcTna3G8nlnRammlNf9ovlqXDzchqbOTUVVU1xvmnR9fmpgLDunBvDYjLB43SOMprkffVH5bnlCwm8zSrHzvdTWkaz3IoNFze9-ern9wZqdeUUlmWSn1kVGiB3CMY2jZKn3SYZg8r2cvlqfTKOAgjuDJxdMpGxDBMeor2mj1qZnrqgTmAUfKG9cznZOUmsQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"One_year_measurements_of_aerosol_optical_properties_over_an_urban_coastal_site_Effect_on_local_direct_radiative_forcing","translated_slug":"","page_count":8,"language":"en","content_type":"Work","summary":"We present results of direct aerosol radiative forcing over a French Mediterranean coastal zone based on one year of continuous observations of aerosol optical properties during 2005-2006. Monthly-mean aerosol optical depth at 440 nm ranged between 0.1 and 0.34, with high Angstrom coefficient (α N 1.2). The single scattering albedo (at 525 nm) estimated at the surface ranged between 0.7 and 0.8, indicating significant absorption. The presence of aerosols over the Mediterranean zone during summer decreases the shortwave radiation reaching the surface by as much as 26 ± 3.9 W m − 2 , and increases the top of the atmosphere reflected radiation by as much as 5.2 ± 1.0 W m − 2. The shortwave atmospheric absorption translates to an atmospheric heating of 2.5 to 4.6 K day − 1. 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As in NAM. the dependence of the aerosol concentration on meteorological parameters is parameterized using empirical coefficients. The effect of continental aerosols present in the coastal zone is modeled as a function of fetch. 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A reasonable agreement is found between the model and the aerosol size distributions as measured on the island Inisheer","owner":{"id":40419649,"first_name":"Jacques","middle_initials":"","last_name":"Piazzola","page_name":"JacquesPiazzola","domain_name":"independent","created_at":"2015-12-20T02:11:32.317-08:00","display_name":"Jacques Piazzola","url":"https://independent.academia.edu/JacquesPiazzola"},"attachments":[{"id":86100463,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/86100463/thumbnails/1.jpg","file_name":"pub95132.pdf","download_url":"https://www.academia.edu/attachments/86100463/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Aerosol_concentration_and_fetch.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/86100463/pub95132-libre.pdf?1652861540=\u0026response-content-disposition=attachment%3B+filename%3DAerosol_concentration_and_fetch.pdf\u0026Expires=1737247636\u0026Signature=gITdJlenMIpT3tg8ZgMPlnWBhAfE1XUZS7md2Q8TK5Uos8SC32WITKf8hfQN9ZfAYWkd~sYjsJQCchGCS32FK81TG0TLc-ZeWrJFU9WwVs8Xxrpj0jIl4gw09jkP29NjQlKnh~h7KZOj~vSyNorx2OCK1~cBrWKKnj58GOuSz1A08Tooj6ziv16-T8DAMeha1JbPrWkbMHA8Pn7vv1PVvV~wCvxMunPMQAlA1hVQXn~a8YFzjj3TXyII3nnc~vE7oXiawFvjyBnNHI4UMzHZYPL8sf9Q8yoilDs4Q1JHLrX-E-FeTXCvMTha0mJlpYv~NzGB3Ilw8VO0Wpg9JWlAwg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":48,"name":"Engineering","url":"https://www.academia.edu/Documents/in/Engineering"},{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":477461,"name":"Coastal Zone","url":"https://www.academia.edu/Documents/in/Coastal_Zone"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358497"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/79358497/The_Advanced_Navy_Aerosol_Model_ANAM_validation_of_small_particle_modes"><img alt="Research paper thumbnail of The Advanced Navy Aerosol Model (ANAM): validation of small-particle modes" class="work-thumbnail" src="https://attachments.academia-assets.com/86100464/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/79358497/The_Advanced_Navy_Aerosol_Model_ANAM_validation_of_small_particle_modes">The Advanced Navy Aerosol Model (ANAM): validation of small-particle modes</a></div><div class="wp-workCard_item"><span>Atmospheric Optics IV: Turbulence and Propagation</span><span>, 2011</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The image quality of electro-optical sensors in the (lower-altitude marine) atmosphere is limited...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The image quality of electro-optical sensors in the (lower-altitude marine) atmosphere is limited by aerosols, which cause contrast reduction due to transmission losses and impact on the thermal signature of objects by scattering solar radiation. The Advanced Navy Aerosol Model (ANAM) aims at providing a quantitative estimate of the aerosol effects on the basis of standard meteorological parameters such as wind speed and relative humidity. For application in coastal regions, the ANAM includes non-marine aerosols that are governed by an ill-defined tuning parameter: the air mass parameter (AMP). The present paper proposes a new parameterization for assessing the effect of these non-marine particles on the propagation. The new parameterization utilizes the Ångström coefficient, which can be experimentally obtained with a sun photometer, and introduces new types of aerosols in ANAM. The new parameterization was tested against experimental validation data acquired at Porquerolles Island at the French Riviera. The limited test data suggested that the new parameterization is only partially efficient in capturing the aerosol signature of the coastal environment. Nevertheless, the new Ångström coefficient algorithm avoids using the ill-defined AMP, and may thus be useful to the ANAM community.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c30b957d8cff29fd91cfd8c4c03517a5" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100464,"asset_id":79358497,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100464/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358497"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358497"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358497; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358497]").text(description); $(".js-view-count[data-work-id=79358497]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358497; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358497']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358497, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "c30b957d8cff29fd91cfd8c4c03517a5" } } $('.js-work-strip[data-work-id=79358497]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358497,"title":"The Advanced Navy Aerosol Model (ANAM): validation of small-particle modes","translated_title":"","metadata":{"publisher":"SPIE","ai_title_tag":"ANAM Validation: New Parameterization for Coastal Aerosols","grobid_abstract":"The image quality of electro-optical sensors in the (lower-altitude marine) atmosphere is limited by aerosols, which cause contrast reduction due to transmission losses and impact on the thermal signature of objects by scattering solar radiation. 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A few years ago, an empirical model was developed describing the aerosol size distributions in the Mediterranean coastal atmosphere near Toulon (France). This model has been coupled with Mie theory to yield the code MEDEX (MEDiterranean EXtinction) for the aerosol extinction. This contribution deals with the evaluation of MEDEX for aerosol data recorded near the Black Sea coast. For this site, MEDEX correctly predicts the aerosol extinction as function of wavelength, albeit with minor discrepancies below one micron. These differences are attributed to the uncertainty in predicting the concentrations of submicron particles. The comparison shows that MEDEX may be more generally applicable than to the Toulon area.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e955d61ed1a591f1e68b4cab71c7e29f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100460,"asset_id":79358496,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100460/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358496"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358496"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358496; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358496]").text(description); $(".js-view-count[data-work-id=79358496]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358496; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358496']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358496, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "e955d61ed1a591f1e68b4cab71c7e29f" } } $('.js-work-strip[data-work-id=79358496]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358496,"title":"Aerosol extinction in coastal zones","translated_title":"","metadata":{"publisher":"SPIE","grobid_abstract":"The performance of electro-optical systems can be substantially affected by aerosol particles that scatter and absorb electromagnetic radiation. A few years ago, an empirical model was developed describing the aerosol size distributions in the Mediterranean coastal atmosphere near Toulon (France). This model has been coupled with Mie theory to yield the code MEDEX (MEDiterranean EXtinction) for the aerosol extinction. This contribution deals with the evaluation of MEDEX for aerosol data recorded near the Black Sea coast. For this site, MEDEX correctly predicts the aerosol extinction as function of wavelength, albeit with minor discrepancies below one micron. These differences are attributed to the uncertainty in predicting the concentrations of submicron particles. 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A few years ago, an empirical model was developed describing the aerosol size distributions in the Mediterranean coastal atmosphere near Toulon (France). This model has been coupled with Mie theory to yield the code MEDEX (MEDiterranean EXtinction) for the aerosol extinction. This contribution deals with the evaluation of MEDEX for aerosol data recorded near the Black Sea coast. For this site, MEDEX correctly predicts the aerosol extinction as function of wavelength, albeit with minor discrepancies below one micron. These differences are attributed to the uncertainty in predicting the concentrations of submicron particles. 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The model that is most frequently used for the prediction of aerosols and their effect on extinction in the marine atmosphere is the U.S. Navy aerosol model (NAM) (Gathman, 1983). The NAM was developed for open ocean applications, where it works well. In coastal areas, however,</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358495"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358495"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358495; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=79358495]").text(description); $(".js-view-count[data-work-id=79358495]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 79358495; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='79358495']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 79358495, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=79358495]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":79358495,"title":"Extension of the Navy aerosol model to coastal areas","translated_title":"","metadata":{"abstract":"The performance assessment of electro-optical systems with propagation prediction codes requires accurate atmospheric models. 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In coastal areas, however,","internal_url":"https://www.academia.edu/79358495/Extension_of_the_Navy_aerosol_model_to_coastal_areas","translated_internal_url":"","created_at":"2022-05-18T00:54:28.425-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":40419649,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Extension_of_the_Navy_aerosol_model_to_coastal_areas","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"The performance assessment of electro-optical systems with propagation prediction codes requires accurate atmospheric models. The model that is most frequently used for the prediction of aerosols and their effect on extinction in the marine atmosphere is the U.S. Navy aerosol model (NAM) (Gathman, 1983). The NAM was developed for open ocean applications, where it works well. In coastal areas, however,","owner":{"id":40419649,"first_name":"Jacques","middle_initials":"","last_name":"Piazzola","page_name":"JacquesPiazzola","domain_name":"independent","created_at":"2015-12-20T02:11:32.317-08:00","display_name":"Jacques Piazzola","url":"https://independent.academia.edu/JacquesPiazzola"},"attachments":[],"research_interests":[{"id":82,"name":"Optical Engineering","url":"https://www.academia.edu/Documents/in/Optical_Engineering"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":5980,"name":"Atmospheric Modeling","url":"https://www.academia.edu/Documents/in/Atmospheric_Modeling"},{"id":263152,"name":"Optical physics","url":"https://www.academia.edu/Documents/in/Optical_physics"},{"id":477461,"name":"Coastal Zone","url":"https://www.academia.edu/Documents/in/Coastal_Zone"},{"id":1237788,"name":"Electrical And Electronic Engineering","url":"https://www.academia.edu/Documents/in/Electrical_And_Electronic_Engineering"},{"id":2313637,"name":"Coastal Area","url":"https://www.academia.edu/Documents/in/Coastal_Area"}],"urls":[{"id":20551562,"url":"http://opticalengineering.spiedigitallibrary.org/article.aspx?articleid=1076180"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="79358494"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/79358494/Marine_aerosol_concentrations_at_different_locations_of_the_northern_hemisphere"><img alt="Research paper thumbnail of Marine aerosol concentrations at different locations of the northern hemisphere" class="work-thumbnail" src="https://attachments.academia-assets.com/86100461/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/79358494/Marine_aerosol_concentrations_at_different_locations_of_the_northern_hemisphere">Marine aerosol concentrations at different locations of the northern hemisphere</a></div><div class="wp-workCard_item"><span>Journal of Aerosol Science</span><span>, 1998</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a453e44925819533dc7f6c62a5e03fb5" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":86100461,"asset_id":79358494,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/86100461/download_file?st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&st=MTczNzI0NDAzNiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="79358494"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="79358494"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 79358494; 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