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redistribution of aerosol particles (APs) during the artificial nucleation and subsequent growth of ice crystals in a supercooled cloud. A significant number of the supercooled cloud droplets during icing periods... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_19352734" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The paper focuses on the redistribution of aerosol particles (APs) during the artificial nucleation and subsequent growth of ice crystals in a supercooled cloud. A significant number of the supercooled cloud droplets during icing periods (seeding agents: C3H8, CO2) did not freeze as was presumed prior to the experiment but instead evaporated. The net mass flux of water vapour from</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/19352734" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="c7151d83582f3148651a365f2630f8df" rel="nofollow" data-download="{"attachment_id":42096485,"asset_id":19352734,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/42096485/download_file?st=MTczMjQyMzU5NSw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="39618295" href="https://independent.academia.edu/StephanMertes">Stephan Mertes</a><script data-card-contents-for-user="39618295" type="text/json">{"id":39618295,"first_name":"Stephan","last_name":"Mertes","domain_name":"independent","page_name":"StephanMertes","display_name":"Stephan Mertes","profile_url":"https://independent.academia.edu/StephanMertes?f_ri=2442","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_19352734 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="19352734"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 19352734, container: ".js-paper-rank-work_19352734", }); 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type="text/json">{"id":5069,"name":"Principal Component Analysis","url":"https://www.academia.edu/Documents/in/Principal_Component_Analysis?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="57433" href="https://www.academia.edu/Documents/in/Seasonality">Seasonality</a>, <script data-card-contents-for-ri="57433" type="text/json">{"id":57433,"name":"Seasonality","url":"https://www.academia.edu/Documents/in/Seasonality?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="60285" href="https://www.academia.edu/Documents/in/Atmospheric_sciences">Atmospheric sciences</a><script data-card-contents-for-ri="60285" type="text/json">{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences?f_ri=2442","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=6463543]'), work: 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type="text/json">{"id":2442,"name":"Atmospheric Science","url":"https://www.academia.edu/Documents/in/Atmospheric_Science?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="60285" href="https://www.academia.edu/Documents/in/Atmospheric_sciences">Atmospheric sciences</a>, <script data-card-contents-for-ri="60285" type="text/json">{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="387782" href="https://www.academia.edu/Documents/in/Urban_Air_Quality">Urban Air Quality</a><script data-card-contents-for-ri="387782" type="text/json">{"id":387782,"name":"Urban Air Quality","url":"https://www.academia.edu/Documents/in/Urban_Air_Quality?f_ri=2442","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=62753770]'), work: {"id":62753770,"title":"Continuous Measurement of Fine and Ultrafine Particulate Matter, Criteria Pollutants and Meteorological Conditions In Urban El Paso, Texas","created_at":"2021-11-30T12:39:47.324-08:00","url":"https://www.academia.edu/62753770/Continuous_Measurement_of_Fine_and_Ultrafine_Particulate_Matter_Criteria_Pollutants_and_Meteorological_Conditions_In_Urban_El_Paso_Texas?f_ri=2442","dom_id":"work_62753770","summary":null,"downloadable_attachments":[{"id":75423175,"asset_id":62753770,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":41614431,"first_name":"Melissa","last_name":"Gonzales","domain_name":"independent","page_name":"MelissaGonzales10","display_name":"Melissa Gonzales","profile_url":"https://independent.academia.edu/MelissaGonzales10?f_ri=2442","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":55,"name":"Environmental Engineering","url":"https://www.academia.edu/Documents/in/Environmental_Engineering?f_ri=2442","nofollow":false},{"id":2442,"name":"Atmospheric Science","url":"https://www.academia.edu/Documents/in/Atmospheric_Science?f_ri=2442","nofollow":false},{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences?f_ri=2442","nofollow":false},{"id":387782,"name":"Urban Air Quality","url":"https://www.academia.edu/Documents/in/Urban_Air_Quality?f_ri=2442","nofollow":false},{"id":391216,"name":"Size Distribution","url":"https://www.academia.edu/Documents/in/Size_Distribution?f_ri=2442"},{"id":518609,"name":"Particulate Matter","url":"https://www.academia.edu/Documents/in/Particulate_Matter?f_ri=2442"},{"id":611814,"name":"Correlation coefficient","url":"https://www.academia.edu/Documents/in/Correlation_coefficient?f_ri=2442"},{"id":1162441,"name":"Ultrafine Particles","url":"https://www.academia.edu/Documents/in/Ultrafine_Particles?f_ri=2442"},{"id":1263981,"name":"Fine Particles","url":"https://www.academia.edu/Documents/in/Fine_Particles?f_ri=2442"},{"id":1290866,"name":"Diurnal Cycle","url":"https://www.academia.edu/Documents/in/Diurnal_Cycle?f_ri=2442"},{"id":2803818,"name":"Atmospheric Environment","url":"https://www.academia.edu/Documents/in/Atmospheric_Environment?f_ri=2442"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_4800237" data-work_id="4800237" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/4800237/Seasonal_characteristics_of_tropical_marine_boundary_layer_air_measured_at_the_Cape_Verde_Atmospheric_Observatory">Seasonal characteristics of tropical marine boundary layer air measured at the Cape Verde Atmospheric Observatory</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Observations of the tropical atmosphere are fundamental to the understanding of global changes in air quality, atmospheric oxidation capacity and climate, yet the tropics are under-populated with long-term measurements. The first three... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_4800237" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Observations of the tropical atmosphere are fundamental to the understanding of global changes in air quality, atmospheric oxidation capacity and climate, yet the tropics are under-populated with long-term measurements. The first three years (October 2006–September 2009) of meteorological, trace gas and particulate data from the global WMO/Global Atmospheric Watch (GAW) Cape Verde Atmospheric Observatory Humberto Duarte Fonseca (CVAO; 16° 51′ N, 24° 52′ W) are presented, along with a characterisation of the origin and pathways of air masses arriving at the station using the NAME dispersion model and simulations of dust deposition using the COSMO-MUSCAT dust model. The observations show a strong influence from Saharan dust in winter with a maximum in super-micron aerosol and particulate iron and aluminium. The dust model results match the magnitude and daily variations of dust events, but in the region of the CVAO underestimate the measured aerosol optical thickness (AOT) because of contributions from other aerosol. The NAME model also captured the dust events, giving confidence in its ability to correctly identify air mass origins and pathways in this region. Dissolution experiments on collected dust samples showed a strong correlation between soluble Fe and Al and measured solubilities were lower at high atmospheric dust concentrations. Fine mode aerosol at the CVAO contains a significant fraction of non-sea salt components including dicarboxylic acids, methanesulfonic acid and aliphatic amines, all believed to be of oceanic origin. A marine influence is also apparent in the year-round presence of iodine and bromine monoxide (IO and BrO), with IO suggested to be confined mainly to the surface few hundred metres but BrO well mixed in the boundary layer. Enhanced CO2 and CH4 and depleted oxygen concentrations are markers for air-sea exchange over the nearby northwest African coastal upwelling area. Long-range transport results in generally higher levels of O3 and anthropogenic non-methane hydrocarbons (NMHC) in air originating from North America. Ozone/CO ratios were highest (up to 0.42) in relatively fresh European air masses. In air heavily influenced by Saharan dust the O3/CO ratio was as low as 0.13, possibly indicating O3 uptake to dust. Nitrogen oxides (NOx and NOy) show generally higher concentrations in winter when air mass origins are predominantly from Africa. High photochemical activity at the site is shown by maximum spring/summer concentrations of OH and HO2 of 9 × 106 molecule cm−3 and 6 × 108 molecule cm−3, respectively. After the primary photolysis source, the most important controls on the HOx budget in this region are IO and BrO chemistry, the abundance of HCHO, and uptake of HOx to aerosol.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/4800237" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="eb1efa2d1a4950802e99cacdbaf60885" rel="nofollow" data-download="{"attachment_id":49628004,"asset_id":4800237,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/49628004/download_file?st=MTczMjQyMzU5NSw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="6199618" href="https://malta.academia.edu/JohnPaulMuscat">John Paul Muscat</a><script data-card-contents-for-user="6199618" type="text/json">{"id":6199618,"first_name":"John Paul","last_name":"Muscat","domain_name":"malta","page_name":"JohnPaulMuscat","display_name":"John Paul Muscat","profile_url":"https://malta.academia.edu/JohnPaulMuscat?f_ri=2442","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_4800237 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="4800237"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 4800237, container: ".js-paper-rank-work_4800237", }); 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$(".js-view-count[data-work-id=4800237]").text(description); $(".js-view-count-work_4800237").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_4800237").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="4800237"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">12</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="896" href="https://www.academia.edu/Documents/in/Air_Quality">Air Quality</a>, <script data-card-contents-for-ri="896" type="text/json">{"id":896,"name":"Air Quality","url":"https://www.academia.edu/Documents/in/Air_Quality?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="2118" href="https://www.academia.edu/Documents/in/Atmospheric_Chemistry">Atmospheric Chemistry</a>, <script data-card-contents-for-ri="2118" type="text/json">{"id":2118,"name":"Atmospheric Chemistry","url":"https://www.academia.edu/Documents/in/Atmospheric_Chemistry?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="2442" href="https://www.academia.edu/Documents/in/Atmospheric_Science">Atmospheric Science</a>, <script data-card-contents-for-ri="2442" type="text/json">{"id":2442,"name":"Atmospheric Science","url":"https://www.academia.edu/Documents/in/Atmospheric_Science?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="11820" href="https://www.academia.edu/Documents/in/Modeling_and_Simulation">Modeling and Simulation</a><script data-card-contents-for-ri="11820" type="text/json">{"id":11820,"name":"Modeling and Simulation","url":"https://www.academia.edu/Documents/in/Modeling_and_Simulation?f_ri=2442","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=4800237]'), work: {"id":4800237,"title":"Seasonal characteristics of tropical marine boundary layer air measured at the Cape Verde Atmospheric Observatory","created_at":"2013-10-17T06:39:02.712-07:00","url":"https://www.academia.edu/4800237/Seasonal_characteristics_of_tropical_marine_boundary_layer_air_measured_at_the_Cape_Verde_Atmospheric_Observatory?f_ri=2442","dom_id":"work_4800237","summary":"Observations of the tropical atmosphere are fundamental to the understanding of global changes in air quality, atmospheric oxidation capacity and climate, yet the tropics are under-populated with long-term measurements. The first three years (October 2006–September 2009) of meteorological, trace gas and particulate data from the global WMO/Global Atmospheric Watch (GAW) Cape Verde Atmospheric Observatory Humberto Duarte Fonseca (CVAO; 16° 51′ N, 24° 52′ W) are presented, along with a characterisation of the origin and pathways of air masses arriving at the station using the NAME dispersion model and simulations of dust deposition using the COSMO-MUSCAT dust model. The observations show a strong influence from Saharan dust in winter with a maximum in super-micron aerosol and particulate iron and aluminium. The dust model results match the magnitude and daily variations of dust events, but in the region of the CVAO underestimate the measured aerosol optical thickness (AOT) because of contributions from other aerosol. The NAME model also captured the dust events, giving confidence in its ability to correctly identify air mass origins and pathways in this region. Dissolution experiments on collected dust samples showed a strong correlation between soluble Fe and Al and measured solubilities were lower at high atmospheric dust concentrations. Fine mode aerosol at the CVAO contains a significant fraction of non-sea salt components including dicarboxylic acids, methanesulfonic acid and aliphatic amines, all believed to be of oceanic origin. A marine influence is also apparent in the year-round presence of iodine and bromine monoxide (IO and BrO), with IO suggested to be confined mainly to the surface few hundred metres but BrO well mixed in the boundary layer. Enhanced CO2 and CH4 and depleted oxygen concentrations are markers for air-sea exchange over the nearby northwest African coastal upwelling area. Long-range transport results in generally higher levels of O3 and anthropogenic non-methane hydrocarbons (NMHC) in air originating from North America. Ozone/CO ratios were highest (up to 0.42) in relatively fresh European air masses. In air heavily influenced by Saharan dust the O3/CO ratio was as low as 0.13, possibly indicating O3 uptake to dust. Nitrogen oxides (NOx and NOy) show generally higher concentrations in winter when air mass origins are predominantly from Africa. High photochemical activity at the site is shown by maximum spring/summer concentrations of OH and HO2 of 9 × 106 molecule cm−3 and 6 × 108 molecule cm−3, respectively. 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href="https://www.academia.edu/13311861/Comparison_of_quantification_methods_to_measure_fire_derived_black_elemental_carbon_in_soils_and_sediments_using_reference_materials_from_soil_water_sediment_and_the_atmosphere">Comparison of quantification methods to measure fire-derived (black/elemental) carbon in soils and sediments using reference materials from soil, water, sediment and the atmosphere</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/13311861" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="a91ef7cb91e88d2874023bb358be14e9" rel="nofollow" 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Science","url":"https://www.academia.edu/Documents/in/Atmospheric_Science?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="60285" href="https://www.academia.edu/Documents/in/Atmospheric_sciences">Atmospheric sciences</a>, <script data-card-contents-for-ri="60285" type="text/json">{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="93298" href="https://www.academia.edu/Documents/in/Fossil_Fuels">Fossil Fuels</a><script data-card-contents-for-ri="93298" type="text/json">{"id":93298,"name":"Fossil Fuels","url":"https://www.academia.edu/Documents/in/Fossil_Fuels?f_ri=2442","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=13311861]'), work: {"id":13311861,"title":"Comparison of quantification methods to measure 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They are a prerequisite for the expression of adverse and hazardous natural phenomena. This report analyses the genesis and location of the adverse and... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_35942256" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The geographical area of Northeastern Bulgaria boasts a specific climate conditions. They are a prerequisite for the expression of adverse and hazardous natural phenomena. This report analyses the genesis and location of the adverse and dangerous meteorological, climate and hydrological phenomena within the Northeastern Bulgaria, which determined by climate conditions.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/35942256" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="e937a47c41d8bf2f9e0383f21d3b5940" rel="nofollow" data-download="{"attachment_id":55824364,"asset_id":35942256,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/55824364/download_file?st=MTczMjQyMzU5NSw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="3432150" href="https://independent.academia.edu/editorijmraus">Publisher ijmra.us UGC Approved</a><script data-card-contents-for-user="3432150" type="text/json">{"id":3432150,"first_name":"Publisher","last_name":"ijmra.us UGC Approved","domain_name":"independent","page_name":"editorijmraus","display_name":"Publisher ijmra.us UGC Approved","profile_url":"https://independent.academia.edu/editorijmraus?f_ri=2442","photo":"https://0.academia-photos.com/3432150/1168016/61177738/s65_publisher.ijmra.us_ugc_approved.gif"}</script></span></span></li><li class="js-paper-rank-work_35942256 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="35942256"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 35942256, container: ".js-paper-rank-work_35942256", }); 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They are a prerequisite for the expression of adverse and hazardous natural phenomena. 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dioxide","url":"https://www.academia.edu/Documents/in/Sulphur_dioxide?f_ri=2442"},{"id":2631981,"name":"Troposphere","url":"https://www.academia.edu/Documents/in/Troposphere?f_ri=2442"},{"id":2803818,"name":"Atmospheric Environment","url":"https://www.academia.edu/Documents/in/Atmospheric_Environment?f_ri=2442"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_58876413" data-work_id="58876413" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/58876413/A_side_by_side_comparison_of_filter_based_PM2_5_measurements_at_a_suburban_site_A_closure_study">A side-by-side comparison of filter-based PM2.5 measurements at a suburban site: A closure study</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x 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data-has-card-for-ri="55" href="https://www.academia.edu/Documents/in/Environmental_Engineering">Environmental Engineering</a>, <script data-card-contents-for-ri="55" type="text/json">{"id":55,"name":"Environmental Engineering","url":"https://www.academia.edu/Documents/in/Environmental_Engineering?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="896" href="https://www.academia.edu/Documents/in/Air_Quality">Air Quality</a>, <script data-card-contents-for-ri="896" type="text/json">{"id":896,"name":"Air Quality","url":"https://www.academia.edu/Documents/in/Air_Quality?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="2442" href="https://www.academia.edu/Documents/in/Atmospheric_Science">Atmospheric Science</a>, <script data-card-contents-for-ri="2442" type="text/json">{"id":2442,"name":"Atmospheric 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Science","url":"https://www.academia.edu/Documents/in/Atmospheric_Science?f_ri=2442","nofollow":false},{"id":16288,"name":"Public Health","url":"https://www.academia.edu/Documents/in/Public_Health?f_ri=2442","nofollow":false},{"id":60056,"name":"Air Sampling","url":"https://www.academia.edu/Documents/in/Air_Sampling?f_ri=2442"},{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences?f_ri=2442"},{"id":98134,"name":"United States","url":"https://www.academia.edu/Documents/in/United_States?f_ri=2442"},{"id":113414,"name":"Uncertainty Estimation","url":"https://www.academia.edu/Documents/in/Uncertainty_Estimation?f_ri=2442"},{"id":392429,"name":"Protocol Specification","url":"https://www.academia.edu/Documents/in/Protocol_Specification?f_ri=2442"},{"id":585192,"name":"Organic carbon","url":"https://www.academia.edu/Documents/in/Organic_carbon?f_ri=2442"},{"id":703835,"name":"Statistical Test","url":"https://www.academia.edu/Documents/in/Statistical_Test?f_ri=2442"},{"id":1131784,"name":"Environmental Protection Agency","url":"https://www.academia.edu/Documents/in/Environmental_Protection_Agency?f_ri=2442"},{"id":2803818,"name":"Atmospheric Environment","url":"https://www.academia.edu/Documents/in/Atmospheric_Environment?f_ri=2442"},{"id":3638863,"name":"Total Carbon","url":"https://www.academia.edu/Documents/in/Total_Carbon?f_ri=2442"},{"id":3641669,"name":"Confidence Level","url":"https://www.academia.edu/Documents/in/Confidence_Level?f_ri=2442"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_35934961" data-work_id="35934961" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/35934961/AN_OVERVIEW_OF_THE_MAJOR_PROCESSES_OF_THE_HYDROLOGIC_CYCLE">AN OVERVIEW OF THE MAJOR PROCESSES OF THE HYDROLOGIC CYCLE</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">This work discusses the continuous movement of water on, above and below the surface of the earth. Brought into focus are the processes of the hydrologic cycle. This study is a useful starting point on the study of hydrology. The cycle... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_35934961" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">This work discusses the continuous movement of water on, above and below the surface of the earth. Brought into focus are the processes of the hydrologic cycle. This study is a useful starting point on the study of hydrology. The cycle begins with the evaporation of water from the ocean due to the heating of the water by the sun's radiation, thereby making it to change to water vapour and driven by air current in the atmosphere to form clouds which later condenses as rain. Processes of hydrological cycle takes place simultaneously at different rates and time. A concise history of the hydrologic cycle was also captured. Evaporation is seen as the major player in the hydrologic cycle.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/35934961" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="af6d37e2700f75e0df270d9979fe41e9" rel="nofollow" data-download="{"attachment_id":55816979,"asset_id":35934961,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/55816979/download_file?st=MTczMjQyMzU5Niw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="3432150" href="https://independent.academia.edu/editorijmraus">Publisher ijmra.us UGC Approved</a><script data-card-contents-for-user="3432150" type="text/json">{"id":3432150,"first_name":"Publisher","last_name":"ijmra.us UGC Approved","domain_name":"independent","page_name":"editorijmraus","display_name":"Publisher ijmra.us UGC Approved","profile_url":"https://independent.academia.edu/editorijmraus?f_ri=2442","photo":"https://0.academia-photos.com/3432150/1168016/61177738/s65_publisher.ijmra.us_ugc_approved.gif"}</script></span></span></li><li class="js-paper-rank-work_35934961 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="35934961"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 35934961, container: ".js-paper-rank-work_35934961", }); 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$(".js-view-count[data-work-id=35934961]").text(description); $(".js-view-count-work_35934961").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_35934961").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="35934961"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">6</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="1200" href="https://www.academia.edu/Documents/in/Languages_and_Linguistics">Languages and Linguistics</a>, <script data-card-contents-for-ri="1200" type="text/json">{"id":1200,"name":"Languages and Linguistics","url":"https://www.academia.edu/Documents/in/Languages_and_Linguistics?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="1512" href="https://www.academia.edu/Documents/in/Climate_Change">Climate Change</a>, <script data-card-contents-for-ri="1512" type="text/json">{"id":1512,"name":"Climate Change","url":"https://www.academia.edu/Documents/in/Climate_Change?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="2442" href="https://www.academia.edu/Documents/in/Atmospheric_Science">Atmospheric Science</a>, <script data-card-contents-for-ri="2442" type="text/json">{"id":2442,"name":"Atmospheric Science","url":"https://www.academia.edu/Documents/in/Atmospheric_Science?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="2549" href="https://www.academia.edu/Documents/in/Hydrology">Hydrology</a><script data-card-contents-for-ri="2549" type="text/json">{"id":2549,"name":"Hydrology","url":"https://www.academia.edu/Documents/in/Hydrology?f_ri=2442","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=35934961]'), work: {"id":35934961,"title":"AN OVERVIEW OF THE MAJOR PROCESSES OF THE HYDROLOGIC CYCLE","created_at":"2018-02-16T00:33:31.698-08:00","url":"https://www.academia.edu/35934961/AN_OVERVIEW_OF_THE_MAJOR_PROCESSES_OF_THE_HYDROLOGIC_CYCLE?f_ri=2442","dom_id":"work_35934961","summary":"This work discusses the continuous movement of water on, above and below the surface of the earth. Brought into focus are the processes of the hydrologic cycle. This study is a useful starting point on the study of hydrology. The cycle begins with the evaporation of water from the ocean due to the heating of the water by the sun's radiation, thereby making it to change to water vapour and driven by air current in the atmosphere to form clouds which later condenses as rain. Processes of hydrological cycle takes place simultaneously at different rates and time. A concise history of the hydrologic cycle was also captured. Evaporation is seen as the major player in the hydrologic cycle.","downloadable_attachments":[{"id":55816979,"asset_id":35934961,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":3432150,"first_name":"Publisher","last_name":"ijmra.us UGC Approved","domain_name":"independent","page_name":"editorijmraus","display_name":"Publisher ijmra.us UGC Approved","profile_url":"https://independent.academia.edu/editorijmraus?f_ri=2442","photo":"https://0.academia-photos.com/3432150/1168016/61177738/s65_publisher.ijmra.us_ugc_approved.gif"}],"research_interests":[{"id":1200,"name":"Languages and Linguistics","url":"https://www.academia.edu/Documents/in/Languages_and_Linguistics?f_ri=2442","nofollow":false},{"id":1512,"name":"Climate Change","url":"https://www.academia.edu/Documents/in/Climate_Change?f_ri=2442","nofollow":false},{"id":2442,"name":"Atmospheric Science","url":"https://www.academia.edu/Documents/in/Atmospheric_Science?f_ri=2442","nofollow":false},{"id":2549,"name":"Hydrology","url":"https://www.academia.edu/Documents/in/Hydrology?f_ri=2442","nofollow":false},{"id":3754,"name":"Climatology","url":"https://www.academia.edu/Documents/in/Climatology?f_ri=2442"},{"id":3755,"name":"Meteorology","url":"https://www.academia.edu/Documents/in/Meteorology?f_ri=2442"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_3228488" data-work_id="3228488" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/3228488/The_Indian_summer_monsoon_rainfall_interplay_of_coupled_dynamics_radiation_and_cloud_microphysics">The Indian summer monsoon rainfall: interplay of coupled dynamics, radiation and cloud microphysics</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/3228488" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="6c292465867fe9127442ef5be7ad60c4" rel="nofollow" data-download="{"attachment_id":31094515,"asset_id":3228488,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/31094515/download_file?st=MTczMjQyMzU5Niw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="3694333" href="https://independent.academia.edu/ToshioYamagata">Toshio Yamagata</a><script data-card-contents-for-user="3694333" type="text/json">{"id":3694333,"first_name":"Toshio","last_name":"Yamagata","domain_name":"independent","page_name":"ToshioYamagata","display_name":"Toshio Yamagata","profile_url":"https://independent.academia.edu/ToshioYamagata?f_ri=2442","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_3228488 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="3228488"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 3228488, container: ".js-paper-rank-work_3228488", }); 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Such a study dealing with ultraviolet and visible wavelengths (310–575 nm) is carried out in Athens for the first time. The... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_25360422" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">This work investigates the seasonal and diurnal variation of total spectral transmittance of solar radiation. Such a study dealing with ultraviolet and visible wavelengths (310–575 nm) is carried out in Athens for the first time. The spectral values presented are averages over a number of records in a period of 42 days and have been calculated using ground-based spectral measurements of direct-beam irradiance. The data were recorded on selected days throughout a year by a simple pyrheliometer capable of performing spectral measurements. All data were recorded under clear-sky conditions in the city center of Athens and the total spectral atmospheric transmittance was estimated in the direction of local zenith to become independent of any optical mass effects. The comparison between seasons reveals that the atmospheric transmittance is higher in the cold period of the year than in the warm, simply because the photochemical pollution in the summer is more severe. Various features of seasonal and diurnal variation are also discussed with respect to emission sources, topographic peculiarities and wind regime.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/25360422" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="41fde8e397f97bb7892783e6bde109fc" rel="nofollow" data-download="{"attachment_id":45661209,"asset_id":25360422,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/45661209/download_file?st=MTczMjQyMzU5Niw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="6418775" href="https://noa.academia.edu/HarryKambezidis">Harry Kambezidis</a><script data-card-contents-for-user="6418775" type="text/json">{"id":6418775,"first_name":"Harry","last_name":"Kambezidis","domain_name":"noa","page_name":"HarryKambezidis","display_name":"Harry Kambezidis","profile_url":"https://noa.academia.edu/HarryKambezidis?f_ri=2442","photo":"https://0.academia-photos.com/6418775/2717680/3164814/s65_harry.kambezidis.jpg"}</script></span></span></li><li class="js-paper-rank-work_25360422 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="25360422"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 25360422, container: ".js-paper-rank-work_25360422", }); });</script></li><li class="js-percentile-work_25360422 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 25360422; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_25360422"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_25360422 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="25360422"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 25360422; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=25360422]").text(description); $(".js-view-count-work_25360422").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_25360422").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="25360422"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">4</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="2442" href="https://www.academia.edu/Documents/in/Atmospheric_Science">Atmospheric Science</a>, <script data-card-contents-for-ri="2442" type="text/json">{"id":2442,"name":"Atmospheric Science","url":"https://www.academia.edu/Documents/in/Atmospheric_Science?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="4884" href="https://www.academia.edu/Documents/in/Atmospheric_Physics">Atmospheric Physics</a>, <script data-card-contents-for-ri="4884" type="text/json">{"id":4884,"name":"Atmospheric Physics","url":"https://www.academia.edu/Documents/in/Atmospheric_Physics?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="8738" href="https://www.academia.edu/Documents/in/Atmospheric_Aerosols">Atmospheric Aerosols</a>, <script data-card-contents-for-ri="8738" type="text/json">{"id":8738,"name":"Atmospheric Aerosols","url":"https://www.academia.edu/Documents/in/Atmospheric_Aerosols?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="284947" href="https://www.academia.edu/Documents/in/Solar_radiation">Solar radiation</a><script data-card-contents-for-ri="284947" type="text/json">{"id":284947,"name":"Solar radiation","url":"https://www.academia.edu/Documents/in/Solar_radiation?f_ri=2442","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=25360422]'), work: {"id":25360422,"title":"Total Atmospheric Transmittance in the UV and VIS Spectra in Athens, Greece","created_at":"2016-05-16T04:23:47.918-07:00","url":"https://www.academia.edu/25360422/Total_Atmospheric_Transmittance_in_the_UV_and_VIS_Spectra_in_Athens_Greece?f_ri=2442","dom_id":"work_25360422","summary":"This work investigates the seasonal and diurnal variation of total spectral transmittance of solar radiation. Such a study dealing with ultraviolet and visible wavelengths (310–575 nm) is carried out in Athens for the first time. The spectral values presented are averages over a number of records in a period of 42 days and have been calculated using ground-based spectral measurements of direct-beam irradiance. The data were recorded on selected days throughout a year by a simple pyrheliometer capable of performing spectral measurements. All data were recorded under clear-sky conditions in the city center of Athens and the total spectral atmospheric transmittance was estimated in the direction of local zenith to become independent of any optical mass effects. The comparison between seasons reveals that the atmospheric transmittance is higher in the cold period of the year than in the warm, simply because the photochemical pollution in the summer is more severe. Various features of seasonal and diurnal variation are also discussed with respect to emission sources, topographic peculiarities and wind regime.","downloadable_attachments":[{"id":45661209,"asset_id":25360422,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":6418775,"first_name":"Harry","last_name":"Kambezidis","domain_name":"noa","page_name":"HarryKambezidis","display_name":"Harry Kambezidis","profile_url":"https://noa.academia.edu/HarryKambezidis?f_ri=2442","photo":"https://0.academia-photos.com/6418775/2717680/3164814/s65_harry.kambezidis.jpg"}],"research_interests":[{"id":2442,"name":"Atmospheric Science","url":"https://www.academia.edu/Documents/in/Atmospheric_Science?f_ri=2442","nofollow":false},{"id":4884,"name":"Atmospheric Physics","url":"https://www.academia.edu/Documents/in/Atmospheric_Physics?f_ri=2442","nofollow":false},{"id":8738,"name":"Atmospheric Aerosols","url":"https://www.academia.edu/Documents/in/Atmospheric_Aerosols?f_ri=2442","nofollow":false},{"id":284947,"name":"Solar radiation","url":"https://www.academia.edu/Documents/in/Solar_radiation?f_ri=2442","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_16259657 coauthored" data-work_id="16259657" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/16259657/The_impact_of_CO2_capture_in_the_power_and_heat_sector_on_the_emission_of_SO2_NOx_particulate_matter_volatile_organic_compounds_and_NH3_in_the_European_Union">The impact of CO2 capture in the power and heat sector on the emission of SO2, NOx, particulate matter, volatile organic compounds and NH3 in the European Union</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/16259657" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="845a7f4082f6946cced176d837c71e42" rel="nofollow" data-download="{"attachment_id":42602347,"asset_id":16259657,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/42602347/download_file?st=MTczMjQyMzU5Niw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa 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InlineList-item-text js-work-more-authors-16259657">+2</span><div class="hidden js-additional-users-16259657"><div><span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a href="https://independent.academia.edu/WimTurkenburg">Wim Turkenburg</a></span></div><div><span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a href="https://independent.academia.edu/AndreFaaij">Andre Faaij</a></span></div></div></span><script>(function(){ var popoverSettings = { el: $('.js-work-more-authors-16259657'), placement: 'bottom', hide_delay: 200, html: true, content: function(){ return $('.js-additional-users-16259657').html(); } } new HoverPopover(popoverSettings); })();</script></li><li class="js-paper-rank-work_16259657 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="16259657"><i class="u-m1x fa fa-bar-chart"></i><strong 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data-work-id="16259657"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 16259657; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=16259657]").text(description); $(".js-view-count-work_16259657").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_16259657").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="16259657"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">13</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="55" href="https://www.academia.edu/Documents/in/Environmental_Engineering">Environmental Engineering</a>, <script data-card-contents-for-ri="55" type="text/json">{"id":55,"name":"Environmental Engineering","url":"https://www.academia.edu/Documents/in/Environmental_Engineering?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="896" href="https://www.academia.edu/Documents/in/Air_Quality">Air Quality</a>, <script data-card-contents-for-ri="896" type="text/json">{"id":896,"name":"Air Quality","url":"https://www.academia.edu/Documents/in/Air_Quality?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="2442" href="https://www.academia.edu/Documents/in/Atmospheric_Science">Atmospheric Science</a>, <script data-card-contents-for-ri="2442" type="text/json">{"id":2442,"name":"Atmospheric Science","url":"https://www.academia.edu/Documents/in/Atmospheric_Science?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="10347" href="https://www.academia.edu/Documents/in/European_Union">European Union</a><script data-card-contents-for-ri="10347" type="text/json">{"id":10347,"name":"European Union","url":"https://www.academia.edu/Documents/in/European_Union?f_ri=2442","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=16259657]'), work: {"id":16259657,"title":"The impact of CO2 capture in the power and heat sector on the emission of SO2, NOx, particulate matter, volatile organic compounds and NH3 in the European Union","created_at":"2015-09-28T03:08:41.431-07:00","url":"https://www.academia.edu/16259657/The_impact_of_CO2_capture_in_the_power_and_heat_sector_on_the_emission_of_SO2_NOx_particulate_matter_volatile_organic_compounds_and_NH3_in_the_European_Union?f_ri=2442","dom_id":"work_16259657","summary":null,"downloadable_attachments":[{"id":42602347,"asset_id":16259657,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":35352523,"first_name":"Joris","last_name":"Koornneef","domain_name":"geologicalsurvey","page_name":"JorisKoornneef","display_name":"Joris Koornneef","profile_url":"https://geologicalsurvey.academia.edu/JorisKoornneef?f_ri=2442","photo":"/images/s65_no_pic.png"},{"id":37075394,"first_name":"Wim","last_name":"Turkenburg","domain_name":"independent","page_name":"WimTurkenburg","display_name":"Wim Turkenburg","profile_url":"https://independent.academia.edu/WimTurkenburg?f_ri=2442","photo":"/images/s65_no_pic.png"},{"id":36933456,"first_name":"Andre","last_name":"Faaij","domain_name":"independent","page_name":"AndreFaaij","display_name":"Andre Faaij","profile_url":"https://independent.academia.edu/AndreFaaij?f_ri=2442","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":55,"name":"Environmental Engineering","url":"https://www.academia.edu/Documents/in/Environmental_Engineering?f_ri=2442","nofollow":false},{"id":896,"name":"Air Quality","url":"https://www.academia.edu/Documents/in/Air_Quality?f_ri=2442","nofollow":false},{"id":2442,"name":"Atmospheric Science","url":"https://www.academia.edu/Documents/in/Atmospheric_Science?f_ri=2442","nofollow":false},{"id":10347,"name":"European Union","url":"https://www.academia.edu/Documents/in/European_Union?f_ri=2442","nofollow":false},{"id":34388,"name":"Power Plant","url":"https://www.academia.edu/Documents/in/Power_Plant?f_ri=2442"},{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences?f_ri=2442"},{"id":146840,"name":"Solid oxide fuel cell","url":"https://www.academia.edu/Documents/in/Solid_oxide_fuel_cell?f_ri=2442"},{"id":445366,"name":"Combined cycle","url":"https://www.academia.edu/Documents/in/Combined_cycle?f_ri=2442"},{"id":518609,"name":"Particulate Matter","url":"https://www.academia.edu/Documents/in/Particulate_Matter?f_ri=2442"},{"id":758278,"name":"Large Scale","url":"https://www.academia.edu/Documents/in/Large_Scale?f_ri=2442"},{"id":1256744,"name":"Organic Compound","url":"https://www.academia.edu/Documents/in/Organic_Compound?f_ri=2442"},{"id":1534685,"name":"Volatile organic compound","url":"https://www.academia.edu/Documents/in/Volatile_organic_compound?f_ri=2442"},{"id":1656539,"name":"Air Pollutants","url":"https://www.academia.edu/Documents/in/Air_Pollutants?f_ri=2442"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_21369290 coauthored" data-work_id="21369290" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/21369290/Non_photic_solar_associations_of_heart_rate_variability_and_myocardial_infarction">Non-photic solar associations of heart rate variability and myocardial infarction</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/21369290" data-share-source="work_strip" 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itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="42452355" href="https://independent.academia.edu/JarmilaSiegelova">Jarmila Siegelova</a><script data-card-contents-for-user="42452355" type="text/json">{"id":42452355,"first_name":"Jarmila","last_name":"Siegelova","domain_name":"independent","page_name":"JarmilaSiegelova","display_name":"Jarmila Siegelova","profile_url":"https://independent.academia.edu/JarmilaSiegelova?f_ri=2442","photo":"/images/s65_no_pic.png"}</script></span></span><span class="u-displayInlineBlock InlineList-item-text"> and <span class="u-textDecorationUnderline u-clickable InlineList-item-text js-work-more-authors-21369290">+1</span><div class="hidden js-additional-users-21369290"><div><span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a href="https://independent.academia.edu/TamaraBreus">Tamara Breus</a></span></div></div></span><script>(function(){ 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function (percentileText) { var container = $(".js-percentile-work_21369290"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_21369290 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="21369290"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 21369290; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=21369290]").text(description); $(".js-view-count-work_21369290").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_21369290").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="21369290"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">14</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="2442" href="https://www.academia.edu/Documents/in/Atmospheric_Science">Atmospheric Science</a>, <script data-card-contents-for-ri="2442" type="text/json">{"id":2442,"name":"Atmospheric Science","url":"https://www.academia.edu/Documents/in/Atmospheric_Science?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="49198" href="https://www.academia.edu/Documents/in/Heart_rate_variability">Heart rate variability</a>, <script data-card-contents-for-ri="49198" type="text/json">{"id":49198,"name":"Heart rate variability","url":"https://www.academia.edu/Documents/in/Heart_rate_variability?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="77582" href="https://www.academia.edu/Documents/in/Space_Weather">Space Weather</a>, <script data-card-contents-for-ri="77582" type="text/json">{"id":77582,"name":"Space Weather","url":"https://www.academia.edu/Documents/in/Space_Weather?f_ri=2442","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="81015" href="https://www.academia.edu/Documents/in/Solar_Activity">Solar Activity</a><script data-card-contents-for-ri="81015" type="text/json">{"id":81015,"name":"Solar Activity","url":"https://www.academia.edu/Documents/in/Solar_Activity?f_ri=2442","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=21369290]'), work: {"id":21369290,"title":"Non-photic solar associations of heart rate variability and 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