{"id":4073,"date":"2021-01-07T12:02:19","date_gmt":"2021-01-07T11:02:19","guid":{"rendered":"https:\/\/www2igg.cnr.it\/?p=4073"},"modified":"2025-11-21T15:11:25","modified_gmt":"2025-11-21T14:11:25","slug":"venezia-2021","status":"publish","type":"post","link":"https:\/\/www.igg.cnr.it\/en\/venezia-2021\/","title":{"rendered":"VENEZIA 2021"},"content":{"rendered":"
Category: <\/span>COMPLETED<\/a>, <\/span>NATIONAL<\/a>, <\/span>PROJECT<\/a><\/div>\n\n\n
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Subsidence of the Venice lagoon and morphological evolution connected to erosive and depositional processes combined with Relative Sea Level Rise<\/h4>\n<\/div>\n\n\n\n
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The loss of elevation above mean sea level is one of the processes with the greatest potential impact on lowland coastal areas. Today, more than ever, it is necessary to continuously update our understanding of subsidence, which is particularly complex in the Venice area due to the specificity of the transitional environment and the variability of the subsurface. Although not as significant in magnitude as in other areas worldwide, subsidence in the area surrounding the Venice lagoon is nevertheless very concerning given the elevation of the land well below mean sea level and the unique nature of the lagoon environment. This research aims to quantify the natural and anthropogenic subsidence of the Venice lagoon, characterizing its geological drivers to simulate the evolution of lagoon environments, taking into account erosional\/depositional and geomechanical processes combined with relative sea level rise (RSLR).
Line 3.1 is coordinated by IGG-CNR and is structured as follows:
\u2013 WP 3.1.3 University of Padua \u2013 Department of Civil, Building and Environmental Engineering University of Padua: \u201cGeomechanical behavior of lagoonal deposits, modeling and development of forecast scenarios for Holocene natural subsidence\u201d
\u2013 WP 3.1.1 National Research Council \u2013 Institute of Geosciences and Earth Resources: \u201cAnalysis of subsidence and vulnerability to Relative Sea Level Rise\u201d
\u2013 WP 3.1.2 OGS - National Institute of Oceanography and Experimental Geophysics: \u201cArchitecture of Late Pleistocene and Holocene deposits\u201d<\/p>\n<\/div>\n\n\n\n

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PROJECT DURATION<\/strong>
11\/2018 – 01\/2023
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CNR CONTACT<\/strong>
Luigi Tosi
luigi.tosi@igg.cnr.it<\/p>\n<\/div>\n<\/div>\n\n\n\n

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FOUNDING<\/strong>
CORILA<\/p>\n<\/div>\n\n\n\n

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EXTERNAL LINK<\/strong>
http:\/\/venezia2021.corila.it\/home\/<\/a><\/p>\n\n\n\n

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FOUNDING
<\/strong>CORILA<\/h6><\/div><\/div><\/div><\/div><\/div>\n\n\n\n
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PROJECT DURATION<\/strong>
11\/2018 – 01\/2023<\/h6><\/div><\/div><\/div><\/div><\/div>\n\n\n\n
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CNR CONTACT
<\/strong>Luigi Tosi
luigi.tosi@igg.cnr.it<\/h6><\/div><\/div><\/div><\/div><\/div>\n\n\n\n
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EXTERNAL LINK
<\/strong>http:\/\/venezia2021.corila.it\/home\/<\/a><\/h6><\/div><\/div><\/div><\/div><\/div>\n<\/div>\n<\/div>","protected":false},"excerpt":{"rendered":"

Subsidnza della laguna di Venezia ed evoluzione morfologica connessa a processi erosivi e deposizionali combinati a Relative Sea Level Rise La perdita di quota altimetrica rispetto al medio mare \u00e8 uno dei processi con potenziale maggiore impatto per le aree costiere di pianura. Oggi pi\u00f9 che mai \u00e8 necessario un continuo aggiornamento delle conoscenze del… <\/p>","protected":false},"author":1,"featured_media":4030,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_eb_attr":"","neve_meta_sidebar":"","neve_meta_container":"contained","neve_meta_enable_content_width":"on","neve_meta_content_width":90,"neve_meta_title_alignment":"","neve_meta_author_avatar":"","neve_post_elements_order":"[\"content\",\"tags\"]","neve_meta_disable_header":"","neve_meta_disable_footer":"","neve_meta_disable_title":"","footnotes":""},"categories":[22,7,14],"tags":[],"post_folder":[25],"class_list":["post-4073","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-concluso","category-nazionale","category-progetti"],"_links":{"self":[{"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/posts\/4073","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/comments?post=4073"}],"version-history":[{"count":5,"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/posts\/4073\/revisions"}],"predecessor-version":[{"id":5454,"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/posts\/4073\/revisions\/5454"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/media\/4030"}],"wp:attachment":[{"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/media?parent=4073"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/categories?post=4073"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/tags?post=4073"},{"taxonomy":"post_folder","embeddable":true,"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/post_folder?post=4073"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}