{"id":45,"date":"2019-03-27T10:28:40","date_gmt":"2019-03-27T10:28:40","guid":{"rendered":"http:\/\/www.cima.ualg.pt\/enlace\/?page_id=45"},"modified":"2023-10-10T16:28:47","modified_gmt":"2023-10-10T16:28:47","slug":"objectives","status":"publish","type":"page","link":"https:\/\/www.cima.ualg.pt\/enlace\/index.php\/objectives\/","title":{"rendered":"Objectives"},"content":{"rendered":"\n<h3 class=\"wp-block-heading\">Project objectives<\/h3>\n\n\n\n<ul class=\"wp-block-list\"><li>Explore process-based models with the aim to identify the best strategy to simulate long-term coastal evolution of sandy coasts.<\/li><li>Explore different approaches to schematize boundary conditions in order to be able to simulate long-term coastal processes.<\/li><li>Develop Duna and ShorelineS models further&#8230;<\/li><li>Create a solution for modeling long-term (years to decades) evolution of sandy coasts integrating marine and aeolian processes, and both cross-shore (1D approach) and longshore (oneline or coastline approach) processes.<\/li><li>Validate the developed approach.<\/li><\/ul>\n\n\n\n<hr class=\"wp-block-separator is-style-wide\"\/>\n\n\n<div id=\"metaslider-id-1162\" style=\"max-width: 800px; margin: 0 auto;\" class=\"ml-slider-3-109-0 metaslider metaslider-responsive metaslider-1162 ml-slider has-dots-nav ms-theme-blend\" role=\"region\" aria-label=\"New Slideshow\" data-height=\"600\" data-width=\"800\">\n    <div id=\"metaslider_container_1162\">\n        <ul id='metaslider_1162' class='rslides'>\n            <li aria-roledescription='slide' aria-labelledby='slide-0'><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.cima.ualg.pt\/enlace\/wp-content\/uploads\/2019\/04\/slider_03-800x600.jpg\" height=\"600\" width=\"800\" alt=\"\" class=\"slider-1162 slide-1215 msDefaultImage\" title=\"slider_03\" \/><div class=\"caption-wrap\"><div class=\"caption\">Fixed dune ridge with a relatively sparse vegetation cover typical of the Mediterranean Biogeographic Region. This ridge features the emerged or subaerial part of the sandy peninsula of Anc\u00e3o in the Ria Formosa, South Portugal<\/div><\/div><\/li>\n            <li style='display: none;' aria-roledescription='slide' aria-labelledby='slide-1'><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.cima.ualg.pt\/enlace\/wp-content\/uploads\/2019\/04\/slider_08-800x600.jpg\" height=\"600\" width=\"800\" alt=\"\" class=\"slider-1162 slide-1212 msDefaultImage\" title=\"slider_08\" \/><div class=\"caption-wrap\"><div class=\"caption\">Colonization and sand fixation of the beach-dune transition by dune plants<\/div><\/div><\/li>\n            <li style='display: none;' aria-roledescription='slide' aria-labelledby='slide-2'><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.cima.ualg.pt\/enlace\/wp-content\/uploads\/2019\/04\/slider_04-800x600.jpg\" height=\"600\" width=\"800\" alt=\"\" class=\"slider-1162 slide-1222 msDefaultImage\" title=\"slider_04\" \/><div class=\"caption-wrap\"><div class=\"caption\">The efficiency of dune plants trapping sediment and building new accretionary features (nebkas)<\/div><\/div><\/li>\n            <li style='display: none;' aria-roledescription='slide' aria-labelledby='slide-3'><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.cima.ualg.pt\/enlace\/wp-content\/uploads\/2019\/04\/slider_010-800x600.jpg\" height=\"600\" width=\"800\" alt=\"\" class=\"slider-1162 slide-1210 msDefaultImage\" title=\"slider_010\" \/><div class=\"caption-wrap\"><div class=\"caption\">Dune grasses growth strategies can keep pace with sand burial<\/div><\/div><\/li>\n            <li style='display: none;' aria-roledescription='slide' aria-labelledby='slide-4'><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.cima.ualg.pt\/enlace\/wp-content\/uploads\/2019\/04\/slider_12-800x600.jpg\" height=\"600\" width=\"800\" alt=\"\" class=\"slider-1162 slide-1223 msDefaultImage\" title=\"slider_12\" \/><div class=\"caption-wrap\"><div class=\"caption\">Retreating shorelines showing high magnitude fresh scarps<\/div><\/div><\/li>\n            <li style='display: none;' aria-roledescription='slide' aria-labelledby='slide-5'><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.cima.ualg.pt\/enlace\/wp-content\/uploads\/2019\/04\/slider_05-800x600.jpg\" height=\"600\" width=\"800\" alt=\"\" class=\"slider-1162 slide-1224 msDefaultImage\" title=\"slider_05\" \/><div class=\"caption-wrap\"><div class=\"caption\">Dune scarps can be covered by sand ramps and ultimately fixed by courageous dune plants<\/div><\/div><\/li>\n            <li style='display: none;' aria-roledescription='slide' aria-labelledby='slide-6'><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.cima.ualg.pt\/enlace\/wp-content\/uploads\/2019\/04\/slider_07-800x600.jpg\" height=\"600\" width=\"800\" alt=\"\" class=\"slider-1162 slide-1214 msDefaultImage\" title=\"slider_07\" \/><div class=\"caption-wrap\"><div class=\"caption\">Beach dynamics, the ability of shorelines of moving rapidly back and forth (note the presence of more than one beach scarp in the image)<\/div><\/div><\/li>\n            <li style='display: none;' aria-roledescription='slide' aria-labelledby='slide-7'><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.cima.ualg.pt\/enlace\/wp-content\/uploads\/2019\/04\/slider_02-800x600.png\" height=\"600\" width=\"800\" alt=\"\" class=\"slider-1162 slide-1217 msDefaultImage\" title=\"slider_02\" \/><div class=\"caption-wrap\"><div class=\"caption\">Rapid response (erosion and recovery) of the emerged beach profile after the impact of storm Emma on 28th February 2018 at Faro Beach, Ria Formosa, South Portugal<\/div><\/div><\/li>\n        <\/ul>\n        \n    <\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>Project objectives Explore process-based models with the aim to identify the best strategy to simulate long-term coastal evolution of sandy coasts. Explore different approaches to schematize boundary conditions in order to be able to simulate long-term coastal processes. Develop Duna and ShorelineS models further&#8230; Create a solution for modeling long-term [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-templates\/template-page-sidebar.php","meta":{"footnotes":""},"class_list":["post-45","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.cima.ualg.pt\/enlace\/index.php\/wp-json\/wp\/v2\/pages\/45","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.cima.ualg.pt\/enlace\/index.php\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.cima.ualg.pt\/enlace\/index.php\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.cima.ualg.pt\/enlace\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.cima.ualg.pt\/enlace\/index.php\/wp-json\/wp\/v2\/comments?post=45"}],"version-history":[{"count":13,"href":"https:\/\/www.cima.ualg.pt\/enlace\/index.php\/wp-json\/wp\/v2\/pages\/45\/revisions"}],"predecessor-version":[{"id":1175,"href":"https:\/\/www.cima.ualg.pt\/enlace\/index.php\/wp-json\/wp\/v2\/pages\/45\/revisions\/1175"}],"wp:attachment":[{"href":"https:\/\/www.cima.ualg.pt\/enlace\/index.php\/wp-json\/wp\/v2\/media?parent=45"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}