{"id":4829,"date":"2020-04-12T00:52:25","date_gmt":"2020-04-11T22:52:25","guid":{"rendered":"http:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/?page_id=4829"},"modified":"2020-12-05T00:53:22","modified_gmt":"2020-12-04T23:53:22","slug":"alexandre-dubois-these","status":"publish","type":"page","link":"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/en\/theses-post-docs\/alexandre-dubois-these\/","title":{"rendered":"Alexandre Dubois (PhD)"},"content":{"rendered":"<div id=\"pl-4829\"  class=\"panel-layout\" ><div id=\"pg-4829-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-4829-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-4829-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div class=\"panel-widget-style panel-widget-style-for-4829-0-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p style=\"text-align: left;\"><span style=\"color: #ffffff;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-5113 size-medium alignleft\" src=\"http:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/P1010435-300x300.jpg\" alt=\"\" width=\"300\" height=\"300\" srcset=\"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/P1010435-300x300.jpg 300w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/P1010435-1024x1025.jpg 1024w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/P1010435-150x150.jpg 150w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/P1010435-768x768.jpg 768w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/P1010435-1536x1536.jpg 1536w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/P1010435-1079x1080.jpg 1079w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/P1010435.jpg 1599w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/span><\/p>\n<h3 style=\"text-align: center;\"><span style=\"color: #ffffff;\">Alexandre Dubois<\/span><\/h3>\n<p>&nbsp;<\/p>\n<p style=\"text-align: left;\">Thesis defended in 2012<br \/>\nin Lorient<br \/>\nPhysical Geography<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-4829-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-4829-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-4829-1-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"1\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h3 style=\"text-align: center;\">Morphodynamic behaviour of pocket beaches in a semi-sheltered meso-tidal environment : example of the Southern beaches of the Rhuys peninsula, Southern Brittany<\/h3>\n<\/div>\n<\/div><\/div><\/div><\/div><div id=\"pg-4829-2\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-4829-2-0\"  class=\"panel-grid-cell\" ><div id=\"panel-4829-2-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"2\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h4 style=\"text-align: left;\"><span style=\"color: #1269b0;\">Abstract<\/span><\/h4>\n<p style=\"text-align: justify;\"><span style=\"color: #4b4b4c;\">Pocket beaches take place along the rocky coastlines. On the Rhuys peninsula, they form protecting sandy barriers at the back low wetlands partially connected to the marine environment. These beaches undergo a strong meso-tidal range, when they are located behind a structural barrier, the ocean swell is strongly attenuated. The local wind generates an important sea of wind whose short frequency waves thus created favour the greatest transverse morphological change and the greatest longitudinal sediment transport. The various hydrodynamic and topographic experiments carried out in the field have highlighted longitudinal sediment transport favoured by a moderate and persistent local wind. With greater agitation, the sedimentary transfers are carried out transversally by more powerful processes of surfing and bank jet. Exchanges take place around a point of equilibrium of lesser activity. Wind and swell have a heterogeneous impact in space. Moreover, the variations in volume clearly indicate that each beach system is independent. No exchange of sediment between beaches is demonstrated, whereas a connection is allowed with the near subtidal domain, between rocky flats. Finally, the degree of impact of a storm depends on its trajectory and the water level. Moreover, the eroded volume is quickly recovered by the system. The sediment budget is preserved. However, with the rise in sea level, dune belts can break with an expected longitudinal redistribution.<\/span><\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"pgc-4829-2-1\"  class=\"panel-grid-cell\" ><div id=\"panel-4829-2-1-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"3\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p style=\"text-align: left; padding-left: 40px;\"><span style=\"color: #1269b0;\"><strong>Supervisors<\/strong><br \/>\n<\/span><span style=\"color: #4b4b4c;\">David Menier<\/span><\/p>\n<p style=\"text-align: left; padding-left: 40px;\"><strong><span style=\"color: #1269b0;\">Keywords<br \/>\n<\/span><\/strong><span style=\"color: #4b4b4c;\">Windwaves<br \/>\nTransversal sand dynamics<br \/>\nMeso-tidal range<br \/>\nBeaches<br \/>\nErosion<br \/>\nLittorals<br \/>\nModifications<br \/>\nFrance<br \/>\nRhuys peninsula<br \/>\n<\/span><\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Alexandre Dubois &nbsp; Th\u00e8se soutenue en 2012 \u00e0 Lorient Domaine de la\u00a0G\u00e9ographie physique Comportement morphodynamique des plages de poche en milieu m\u00e9sotidal semi-abrit\u00e9 : exemple des plages m\u00e9ridionales de la presqu\u2019\u00eele de Rhuys, Bretagne sud<\/p>","protected":false},"author":9,"featured_media":5114,"parent":3951,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-4829","page","type-page","status-publish","has-post-thumbnail","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.7 - 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