{"id":20,"date":"2008-12-14T14:23:26","date_gmt":"2008-12-14T14:23:26","guid":{"rendered":"https:\/\/moutinpress.yadlapomme.com\/frcycle-du-carbone-et-climatennouvel-article\/"},"modified":"2026-05-20T08:48:50","modified_gmt":"2026-05-20T06:48:50","slug":"cycle-du-carbone-et-climat","status":"publish","type":"page","link":"https:\/\/thierry-moutin.fr\/en\/teaching\/carbone-cycle-and-climate\/","title":{"rendered":"Carbone cycle and climate"},"content":{"rendered":"\r\n<h2 class=\"wp-block-heading\"><strong>T. Moutin &amp; H. Claustre, C. Lo Monaco, L. Bopp, I. Xueref-R\u00e9mi, D. Lefevre, F. Lemoigne, C. Tamburini<\/strong> (M2S1)<\/h2>\r\n\r\n\r\n\r\n<p class=\"wp-block-paragraph\"><strong>Objective<\/strong><\/p>\r\n\r\n\r\n\r\n<p class=\"wp-block-paragraph\">The aim of this lecture is to lay the foundations for the role of the marine carbon cycle in controlling climate on a global scale by regulating the partial pressure of atmospheric CO<sub>2<\/sub>.\r\nThe course covers the carbon cycle in the surface ocean and water column, the calcium carbonate cycle, glacial and interglacial fluctuations in atmospheric CO<sub>2<\/sub> during the Holocene, and anthropogenic CO<sub>2<\/sub> perturbation (methods for tracing anthropogenic carbon in the ocean).<\/p>\r\n\r\n\r\n<div class=\"wp-block-image\">\r\n<figure class=\"aligncenter\"><img loading=\"lazy\" decoding=\"async\" width=\"661\" height=\"366\" src=\"https:\/\/thierry-moutin.fr\/wp-content\/uploads\/2008\/12\/Image_OPCB348-1.png\" alt=\"Image_OPCB348.png\" class=\"wp-image-19\" srcset=\"https:\/\/thierry-moutin.fr\/wp-content\/uploads\/2008\/12\/Image_OPCB348-1.png 661w, https:\/\/thierry-moutin.fr\/wp-content\/uploads\/2008\/12\/Image_OPCB348-1-300x166.png 300w\" sizes=\"auto, (max-width: 661px) 100vw, 661px\" \/><\/figure>\r\n<\/div>\r\n\r\n\r\n<p class=\"wp-block-paragraph\">Map showing annual mean air-sea CO2 partial pressure difference, based on data from Takahashi et al. 2002 (from Sarmiento &amp; Gruber, 2006).<\/p>\r\n\r\n\r\n\r\n<p class=\"wp-block-paragraph\"><strong>Lectures<\/strong><\/p>\r\n\r\n\r\n\r\n<p class=\"wp-block-paragraph\">1. The carbon cycle in the surface ocean<\/strong>: what factors control pCO2 in the surface ocean (dissolved mineral carbon chemistry &#8211; Revelle factor, mean annual distribution &#8211; physical and biological control processes, seasonal variability &#8211; subtropical gyres, North Atlantic, North Pacific), case study (deep-sea upwelling).<\/p>\r\n\r\n\r\n\r\n<p class=\"wp-block-paragraph\">2. The carbon cycle in the water column<\/strong> (notion of pump, biological pumps, solubility or gas exchange pump, model results),<\/p>\r\n\r\n\r\n\r\n<p class=\"wp-block-paragraph\">3. The calcium carbonate cycle<\/strong> (formation, processes in the water column &#8211; CaCO3 solubility, saturation state, carbonate distribution, dissolution in the water column -, impact of ocean acidification),<\/p>\r\n\r\n\r\n\r\n<p class=\"wp-block-paragraph\">4. Anthropogenic CO<sub>2<\/sub> perturbation<\/strong> (the greenhouse effect, glacial-interglacial fluctuations in atmospheric CO<sub>2<\/sub> during the Holocene, global warming, evidence of anthropogenic perturbation). Thermodynamic and kinetic constraints on CO<sub>2<\/sub> transfer between atmosphere and ocean. Penetration of anthropogenic CO<sub>2<\/sub> into the ocean (direct estimates, methods for tracing anthropogenic carbon in the ocean &#8211; TROCA method, C* method, Chen and Millero method -, current and future ocean absorption capacity).<\/p>\r\n\r\n\r\n\r\n<p class=\"wp-block-paragraph\"><strong>Other Interventions<\/strong><\/p>\r\n\r\n\r\n\r\n<p class=\"wp-block-paragraph\"><a href=\"https:\/\/www.researchgate.net\/profile\/Claire-Lo-Monaco\">Claire Lo Monaco<\/a> (CNAP, LOCEAN Paris) previously N. Metzl (same laboratory, DR, Head of SOLAS-IMBER carbon group): &#8220;Evolution of oceanic CO<sub>2<\/sub> in the South Indian Ocean (OISO campaigns)&#8221;<\/p>\r\n\r\n\r\n\r\n<p class=\"wp-block-paragraph\"><a href=\"https:\/\/lov.imev-mer.fr\/web\/member\/herve-claustre\/\">Herv\u00e9 Claustre <\/a>(DR CNRS Villefranche\/mer, Chairman of the international Bio-Argo working group. Project leader: Remotely-sensed biogeochemical cycles in the Ocean): &#8220;Carbon balances at global, regional and local scales: contribution of sea color remote sensing and instrumented autonomous platforms&#8221;<\/p>\r\n\r\n\r\n\r\n<p class=\"wp-block-paragraph\"><a href=\"https:\/\/savoirs.ens.fr\/conferencier.php?id=2393\">Laurent Bopp <\/a>(Department Director at ENS Paris): Modeling Marine Biogeochemistry. Applications to climate change<\/p>\r\n\r\n\r\n\r\n<p class=\"wp-block-paragraph\"><a href=\"https:\/\/www-iuem.univ-brest.fr\/lemar\/equipe\/le-moigne_frederic\/\">Fr\u00e9d\u00e9ric Lemoigne<\/a> (CR CNRS Brest) and <a href=\"https:\/\/people.mio.osupytheas.fr\/tamburini.christian\/\">Christian Tamburini <\/a>(DR CNRS Marseille) : &#8220;Efficiency of the biological pump in the transfer of matter and carbon in the epi- and mesopelagic zone, Role of dissolved organic carbon in the oceanic carbon cycle&#8221;<\/p>\r\n\r\n\r\n\r\n<p class=\"wp-block-paragraph\"><a href=\"https:\/\/people.mio.osupytheas.fr\/lefevre.dominique\/\">Dominique Lef\u00e8vre<\/a> (CR CNRS Marseille) : &#8220;Biological pump and dissolved oxygen dynamics&#8221;<\/p>\r\n\r\n\r\n\r\n<p class=\"wp-block-paragraph\"><a href=\"https:\/\/www.imbe.fr\/irene-xueref-remy.html\">Ir\u00e8ne Xueref-R\u00e9mi<\/a> (CNAP, Marseille) : &#8220;Assessment of CO2 stocks and fluxes in the atmosphere&#8221;<\/p>\r\n","protected":false},"excerpt":{"rendered":"<p>T. Moutin &amp; H. Claustre, C. Lo Monaco, L. Bopp, I. Xueref-R\u00e9mi, D. Lefevre, F. Lemoigne, C. Tamburini (M2S1) Objective The aim of this lecture is to lay the foundations for the role of the marine carbon cycle in controlling climate on a global scale by regulating the partial pressure of atmospheric CO2. The course &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/thierry-moutin.fr\/en\/teaching\/carbone-cycle-and-climate\/\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;Carbone cycle and climate&#8221;<\/span><\/a><\/p>\n","protected":false},"author":2,"featured_media":0,"parent":89,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"categories":[10],"tags":[],"class_list":["post-20","page","type-page","status-publish","hentry","category-master"],"_links":{"self":[{"href":"https:\/\/thierry-moutin.fr\/en\/wp-json\/wp\/v2\/pages\/20","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/thierry-moutin.fr\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/thierry-moutin.fr\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/thierry-moutin.fr\/en\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/thierry-moutin.fr\/en\/wp-json\/wp\/v2\/comments?post=20"}],"version-history":[{"count":4,"href":"https:\/\/thierry-moutin.fr\/en\/wp-json\/wp\/v2\/pages\/20\/revisions"}],"predecessor-version":[{"id":2040,"href":"https:\/\/thierry-moutin.fr\/en\/wp-json\/wp\/v2\/pages\/20\/revisions\/2040"}],"up":[{"embeddable":true,"href":"https:\/\/thierry-moutin.fr\/en\/wp-json\/wp\/v2\/pages\/89"}],"wp:attachment":[{"href":"https:\/\/thierry-moutin.fr\/en\/wp-json\/wp\/v2\/media?parent=20"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/thierry-moutin.fr\/en\/wp-json\/wp\/v2\/categories?post=20"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/thierry-moutin.fr\/en\/wp-json\/wp\/v2\/tags?post=20"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}