{"id":4824,"date":"2020-04-12T00:41:55","date_gmt":"2020-04-11T22:41:55","guid":{"rendered":"http:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/?page_id=4824"},"modified":"2023-12-20T12:11:10","modified_gmt":"2023-12-20T11:11:10","slug":"ismail-aouiche-these","status":"publish","type":"page","link":"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/en\/theses-post-docs\/ismail-aouiche-these\/","title":{"rendered":"Ismail Aouiche (PhD)"},"content":{"rendered":"<div id=\"pl-4824\"  class=\"panel-layout\" ><div id=\"pg-4824-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-4824-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-4824-0-0-0\" 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-4824-0-0-0\" ><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;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-4725 alignleft\" src=\"http:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/s200_ismail.aouiche.jpg\" alt=\"\" width=\"300\" height=\"300\" srcset=\"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/s200_ismail.aouiche.jpg 200w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/s200_ismail.aouiche-150x150.jpg 150w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/p>\n<h3 style=\"text-align: center;\"><span style=\"color: #ffffff;\">Ismail Aouiche<\/span><\/h3>\n<p>&nbsp;<\/p>\n<p style=\"text-align: left;\">Thesis defended on May 20th 2016<br \/>\nin Aix-Marseille<br \/>\nGeography<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-4824-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-4824-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-4824-1-0-0\" 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;\">Sediment morpho dynamics of the bay of Agadir : multi-method approach and recommendations for an integrated management of the coastal zone<\/h3>\n<\/div>\n<\/div><\/div><\/div><\/div><div id=\"pg-4824-2\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-4824-2-0\"  class=\"panel-grid-cell\" ><div id=\"panel-4824-2-0-0\" 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;\">Coastal systems where sediment transport is perturbed by engineering interventions on the shoreline and shoreface commonly provide fine examples liable to throw light on these links. This is especially so where shoreface bathymetric datasets, which are generally lacking, are collected over time, enabling more or less fine resolution of the meso-scale coastal sediment budget. Agadir Bay and the city of Agadir together form one of the two most important economic development poles on the Atlantic coast of Morocco. Using a combined methodological approach based on wave\u2013current modelling, bathymetric chart-differencing, determination of shoreline fluctuations, and beach topographic surveying, we highlight the close links between variations in the bed of the inner shoreface and the bay shoreline involving both cross-shore and longshore sand transport pathways, sediment budget variations and new sediment cell patterns. This work discusses also the morphological changes and evolution of Agadir Bay beach (Morocco) in response to eight storms between January 2014 and March 2014. A comparison is carried out of the evolution and variability of the beach in a sector of the bay protected by the commercial harbour of Agadir relative to a sector down drift of the harbour that is more exposed to waves, and changes affecting the beach following these storms are examined. Wave influence is evaluated using numerical simulations. The results show that despite being of relatively low intensity, the two first storm events, and especially storm 1, are responsible for major beach morphological changes.<\/span><\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"pgc-4824-2-1\"  class=\"panel-grid-cell\" ><div id=\"panel-4824-2-1-0\" 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=\"padding-left: 40px;\"><a href=\"http:\/\/www.theses.fr\/2016AIXM3017\/document\" target=\"_blank\" rel=\"noopener\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-4805\" src=\"http:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/icons8-document-500_blue-1-300x300.png\" alt=\"\" width=\"100\" height=\"100\" srcset=\"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/icons8-document-500_blue-1-300x300.png 300w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/icons8-document-500_blue-1-150x150.png 150w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/icons8-document-500_blue-1.png 500w\" sizes=\"auto, (max-width: 100px) 100vw, 100px\" \/><\/a><\/p>\n<p style=\"text-align: left; padding-left: 40px;\"><span style=\"color: #1269b0;\"><strong>Supervisors<\/strong><br \/>\n<\/span><span style=\"color: #4b4b4c;\">Mouncef Sedrati<br \/>\nEdward Anthony<br \/>\nLahcen Daoudi <\/span><\/p>\n<p style=\"padding-left: 40px;\"><strong><span style=\"color: #1269b0;\">President of the jury<br \/>\n<\/span><\/strong><span style=\"color: #4b4b4c;\">Bendahhou Zourarah<\/span><\/p>\n<p style=\"padding-left: 40px;\"><strong><span style=\"color: #1269b0;\">Members of the jury<br \/>\n<\/span><\/strong><span style=\"color: #4b4b4c;\">Ali Rhoujjati<\/span><\/p>\n<p style=\"padding-left: 40px;\"><strong><span style=\"color: #1269b0;\">Rapporteurs<\/span><\/strong><br \/>\n<span style=\"color: #4b4b4c;\">Bruno Castelle<br \/>\n<\/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;\">Numeric simulation<br \/>\nSediment cell<br \/>\nStorms<br \/>\nCoastal systems<br \/>\nAgadir Bay<br \/>\nSediment budget<br \/>\nModifications<br \/>\nLittorals<br \/>\nMorocco<br \/>\nAgadir<\/span><\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Ismail Aouiche &nbsp; Th\u00e8se soutenue le 20-05-2016 \u00e0 Aix-Marseille Domaine de G\u00e9ographie Dynamique morphos\u00e9dimentaire de la baie d\u2019Agadir : approche multi-m\u00e9thodes et pr\u00e9conisations pour une gestion int\u00e9gr\u00e9e de la zone c\u00f4ti\u00e8re<\/p>","protected":false},"author":9,"featured_media":4828,"parent":3951,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-4824","page","type-page","status-publish","has-post-thumbnail","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.4 - 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