{"id":18762,"date":"2025-01-20T21:12:23","date_gmt":"2025-01-20T20:12:23","guid":{"rendered":"https:\/\/www.mio.osupytheas.fr\/?page_id=18762"},"modified":"2025-02-25T12:09:48","modified_gmt":"2025-02-25T11:09:48","slug":"flows-at-the-air-sea-interface","status":"publish","type":"page","link":"https:\/\/www.mio.osupytheas.fr\/en\/recherche\/les-equipes-de-recherche\/equipe-oceanographie-physique-littorale-et-cotiere-oplc\/flux-a-linterface-air-mer\/","title":{"rendered":"Flow at the air\/sea interface"},"content":{"rendered":"\t\t<div data-elementor-type=\"wp-page\" data-elementor-id=\"18762\" class=\"elementor elementor-18762\" data-elementor-post-type=\"page\">\n\t\t\t\t<div class=\"elementor-element elementor-element-6f7d44d e-flex e-con-boxed e-con e-parent\" data-id=\"6f7d44d\" data-element_type=\"container\" data-e-type=\"container\" data-settings=\"{&quot;background_background&quot;:&quot;classic&quot;}\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t<div class=\"elementor-element elementor-element-3e04797f e-flex e-con-boxed e-con e-child\" data-id=\"3e04797f\" data-element_type=\"container\" data-e-type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-24365c9a elementor-widget__width-initial elementor-widget elementor-widget-theme-post-title elementor-page-title elementor-widget-heading\" data-id=\"24365c9a\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"theme-post-title.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<h1 class=\"elementor-heading-title elementor-size-default\">Flux \u00e0 l&#8217;interface air\/mer<\/h1>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-1e2503c2 elementor-widget__width-initial breadcrumb elementor-widget elementor-widget-shortcode\" data-id=\"1e2503c2\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"shortcode.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<div class=\"elementor-shortcode\"><nav aria-label=\"breadcrumbs\">\n            <div class=\"breadcrumb-container theme1\">\n                <ol>\n                                    <\/ol>\n            <\/div>\n        <\/nav>    <script type=\"application\/ld+json\">\n        {\n            \"@context\": \"http:\/\/schema.org\",\n            \"@type\": \"BreadcrumbList\",\n            \"itemListElement\": [\n                            ]\n        }\n    <\/script>\n   \n    <script>\n            <\/script>\n <\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-9163c8e e-flex e-con-boxed e-con e-parent\" data-id=\"9163c8e\" data-element_type=\"container\" data-e-type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-9efa5ea elementor-widget elementor-widget-text-editor\" data-id=\"9efa5ea\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>\u00a0<\/p><p style=\"text-align: justify;\">Les travaux de l&#8217;\u00e9quipe s&#8217;articulent autour d&#8217;une meilleure compr\u00e9hension et mod\u00e9lisation des flux turbulents \u00e0 l\u2019interface air-mer et de la dynamique atmosph\u00e9rique en zone c\u00f4ti\u00e8re, ainsi que les cons\u00e9quences sur les propri\u00e9t\u00e9s et la m\u00e9t\u00e9orologie de la couche limite atmosph\u00e9rique marine. Ceci inclut l&#8217;\u00e9tude de l\u2019\u00e9volution du couplage vent-vagues, du d\u00e9ferlement (macro et micro-\u00e9chelle), de la fonction source de l\u2019a\u00e9rosol marin et son transport dans la basse couche atmosph\u00e9rique.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-4de430e e-flex e-con-boxed e-con e-parent\" data-id=\"4de430e\" data-element_type=\"container\" data-e-type=\"container\" data-settings=\"{&quot;background_background&quot;:&quot;classic&quot;}\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-af0657c elementor-widget elementor-widget-heading\" data-id=\"af0657c\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<h3 class=\"elementor-heading-title elementor-size-default\">Publications r\u00e9centes<\/h3>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-de026ce e-flex e-con-boxed e-con e-parent\" data-id=\"de026ce\" data-element_type=\"container\" data-e-type=\"container\" data-settings=\"{&quot;background_background&quot;:&quot;classic&quot;}\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-0bc7343 elementor-widget elementor-widget-text-editor\" data-id=\"0bc7343\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p style=\"text-align: justify;\"><em>Physicochemical Characterization of Aerosols in the Coastal Zone: Evidence of Persistent Carbon Soot in the Marine Atmospheric Boundary Layer (MABL)<\/em> &#8230;,&#8230;, D Ferry, A Limoges, T Missamou, J Piazzola &#8211; Atmosphere, 2023 \u2013 mdpi.com.<\/p><p style=\"text-align: justify;\"><em>Atmospheric sea spray modeling in the North-East Atlantic Ocean using tunnel-derived generation functions and the SUMOS cruise data set<\/em>, &#8230;, MJ van Eijk, T Missamou, J Piazzola &#8211; Journal of Geophysical &#8230;, 2023 \u2013 hal.science.<\/p><p style=\"text-align: justify;\"><em>A Modeling Framework of Atmospheric CO2 in the Mediterranean Marseille Coastal City Area, France<\/em>, &#8230;, T Lauvaux, C Yohia, D Piga, J Piazzola&#8230; &#8211; Atmosphere, 2024 \u2013 mdpi.com.<\/p><p style=\"text-align: justify;\"><em>Study of the Atmospheric Transport of Sea-Spray Aerosols in a Coastal Zone Using a High-Resolution Model<\/em>, A Limoges, J Piazzola, C Yohia, Q Rodier, W Bruch&#8230; &#8211; Atmosphere, 2024 \u2013 mdpi.com.<\/p><p style=\"text-align: justify;\"><em>Analysis of atmospheric CO2 variability in the Marseille city area and the north-west Mediterranean basin at different time scales<\/em>, &#8230;, PE Blanc, C Yohia, J Piazzola&#8230; &#8211; Atmospheric &#8230;, 2023 \u2013 Elsevier.<\/p><p style=\"text-align: justify;\"><em>High-resolution modeling of the spatiotemporal variations in aerosol extinction in a complex coastal area<\/em>, &#8230;, Q Rodier, AMJ van Eijk, J Piazzola &#8211; &#8230; Effects on Light &#8230;, 2023 \u2013 spiedigitallibrary.org.<\/p><p style=\"text-align: justify;\"><em>Numerical simulation of sea spray turbulent transport at the marine boundary layer<\/em>, &#8230;, K Rocha-Brownell, S Wells, W Bruch, J Piazzola&#8230; &#8211; Bulletin of the American &#8230;, 2022 \u2013 APS.<\/p><p style=\"text-align: justify;\"><em>Surface measurements for oceanographic satellites-sea spray aerosols<\/em>, W Bruch, S Peter, M Tathy, A van Eijk, J Piazzola \u2013 2023.<\/p><p style=\"text-align: justify;\"><em>Estimation of the Eddy Viscosity Profile in the Sea Surface Boundary Layer from Underway ADCP Observations<\/em>, A Sentchev, M Yaremchuk, D Bourras&#8230; &#8211; &#8230; of Atmospheric and &#8230;, 2023 \u2013 journals.ametsoc.org.<\/p><p style=\"text-align: justify;\"><em>Comparison of ERA5 turbulent fluxes at the air\u2013sea interface with measurements from a wave\u2010following platform<\/em>, S Benjeddou, D Bourras, C Luneau &#8211; Atmospheric and Oceanic Science &#8230;, 2024 \u2013 Elsevier.<\/p><p style=\"text-align: justify;\"><em>Exchanges of Kinetic Energy at the Ocean-Atmosphere Interface: A closer look at the Wave-influenced Boundary Layer (WBL) from wind-wave tank data and from a<\/em> &#8230;P Frauni\u00e9, D Bourras &#8211; WAVES AND VORTICES IN COMPLEX MEDIA &#8230;, 2022 &#8211; hal.science.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-c53e4c2 e-flex e-con-boxed e-con e-parent\" data-id=\"c53e4c2\" data-element_type=\"container\" data-e-type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-f633a6e elementor-widget elementor-widget-heading\" data-id=\"f633a6e\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<h3 class=\"elementor-heading-title elementor-size-default\">Projets en cours<\/h3>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-8f0c008 e-flex e-con-boxed e-con e-parent\" data-id=\"8f0c008\" data-element_type=\"container\" data-e-type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-d78d14b elementor-widget elementor-widget-text-editor\" data-id=\"d78d14b\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p style=\"text-align: justify;\"><strong>ANR ASTRID PRAMAG<\/strong> : (PI : Boris Conan LEHAA), 99k\u20ac MIO. \u00c9tude du profil de vent dans la couche limite marine oc\u00e9anique de surface et analyse des \u00e9carts entre des profils mesur\u00e9s par LIDAR et ceux issus de la th\u00e9orie de Monin-Obulhov, en fonction des caract\u00e9ristiques des vagues et de la stratification thermique de l&#8217;atmosph\u00e8re.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t<div class=\"elementor-element elementor-element-4c0b8737 e-flex e-con-boxed e-con e-parent\" data-id=\"4c0b8737\" data-element_type=\"container\" data-e-type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-4fe4536f elementor-widget elementor-widget-heading\" data-id=\"4fe4536f\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<span class=\"elementor-heading-title elementor-size-default\">Partager sur 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16.3-30.3 1.8-3.7.9-6.9-.5-9.7-1.4-2.8-12.5-30.1-17.1-41.2-4.5-10.8-9.1-9.3-12.5-9.5-3.2-.2-6.9-.2-10.6-.2-3.7 0-9.7 1.4-14.8 6.9-5.1 5.6-19.4 19-19.4 46.3 0 27.3 19.9 53.7 22.6 57.4 2.8 3.7 39.1 59.7 94.8 83.8 35.2 15.2 49 16.5 66.6 13.9 10.7-1.6 32.8-13.4 37.4-26.4 4.6-13 4.6-24.1 3.2-26.4-1.3-2.5-5-3.9-10.5-6.6z\"><\/path><\/svg>\t\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"<p>\u00a0Les travaux de l&#8217;\u00e9quipe s&#8217;articulent autour d&#8217;une meilleure compr\u00e9hension et mod\u00e9lisation des flux turbulents \u00e0 l\u2019interface air-mer et de la dynamique atmosph\u00e9rique en zone c\u00f4ti\u00e8re, ainsi que les cons\u00e9quences sur [&hellip;]<\/p>\n","protected":false},"author":319,"featured_media":4489,"parent":18697,"menu_order":3,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-18762","page","type-page","status-publish","has-post-thumbnail","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/pages\/18762","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/users\/319"}],"replies":[{"embeddable":true,"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/comments?post=18762"}],"version-history":[{"count":17,"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/pages\/18762\/revisions"}],"predecessor-version":[{"id":19565,"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/pages\/18762\/revisions\/19565"}],"up":[{"embeddable":true,"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/pages\/18697"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/media\/4489"}],"wp:attachment":[{"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/media?parent=18762"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}