{"id":85,"date":"2021-09-21T11:15:30","date_gmt":"2021-09-21T10:15:30","guid":{"rendered":"https:\/\/www.master-planeto.universite-paris-saclay.fr\/?page_id=85"},"modified":"2022-02-19T12:11:45","modified_gmt":"2022-02-19T11:11:45","slug":"ue-10-systemes-climatiques-et-evolution-des-surfaces-planetaires","status":"publish","type":"page","link":"https:\/\/www.master-planeto.universite-paris-saclay.fr\/?page_id=85","title":{"rendered":"UE 10 &#8211; Syst\u00e8mes climatiques et \u00e9volution des surfaces plan\u00e9taires"},"content":{"rendered":"\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/www.master-planeto.universite-paris-saclay.fr\/wp-content\/uploads\/2022\/02\/pluton_new_horizons.jpg\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"437\" src=\"https:\/\/www.master-planeto.universite-paris-saclay.fr\/wp-content\/uploads\/2022\/02\/pluton_new_horizons-1024x437.jpg\" alt=\"\" class=\"wp-image-617\" srcset=\"https:\/\/www.master-planeto.universite-paris-saclay.fr\/wp-content\/uploads\/2022\/02\/pluton_new_horizons-1024x437.jpg 1024w, https:\/\/www.master-planeto.universite-paris-saclay.fr\/wp-content\/uploads\/2022\/02\/pluton_new_horizons-300x128.jpg 300w, https:\/\/www.master-planeto.universite-paris-saclay.fr\/wp-content\/uploads\/2022\/02\/pluton_new_horizons-768x328.jpg 768w, https:\/\/www.master-planeto.universite-paris-saclay.fr\/wp-content\/uploads\/2022\/02\/pluton_new_horizons-1536x656.jpg 1536w, https:\/\/www.master-planeto.universite-paris-saclay.fr\/wp-content\/uploads\/2022\/02\/pluton_new_horizons.jpg 1920w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption><em>L&rsquo;atmosph\u00e8re et les glaciers de Pluton r\u00e9v\u00e9l\u00e9s par la sonde New Horizons (2015) <\/em><\/figcaption><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">Ce module interdisciplinaire (climatologie\/g\u00e9ologie) a pour objectif de pr\u00e9senter les environnements et les atmosph\u00e8res sur diff\u00e9rents mondes du syst\u00e8me solaire et de d\u00e9crire les processus physiques qui contr\u00f4lent les climats et comment ils fa\u00e7onnent les surfaces plan\u00e9taires . Cela permet d&rsquo;illustrer des concepts th\u00e9oriques par des exemple observ\u00e9s, tout en restant au plus pr\u00e8s des probl\u00e8mes de recherche actuels et des d\u00e9bats en cours. <\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Les cours sont donn\u00e9s par des sp\u00e9cialistes \u00e0 la pointe de la recherche sur les sujets enseign\u00e9s: Fran\u00e7ois Forget, Sandrine Guerlet, Jean-Baptiste Madeleine, S\u00e9bastien Lebonnois, Nicolas Mangold, Antoine S\u00e9journ\u00e9.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\">Contenu du module<\/h3>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>1 &#8211; <\/strong> <strong><strong>Le syst\u00e8me climatique de la plan\u00e8te Mars<\/strong><\/strong> <br><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/planeto.geol.u-psud.fr\/local\/cache-vignettes\/L8xH11\/puce-32883.gif\" alt=\"-\" width=\"8\" height=\"11\">&nbsp;Dynamique atmosph\u00e9rique<br><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/planeto.geol.u-psud.fr\/local\/cache-vignettes\/L8xH11\/puce-32883.gif\" alt=\"-\" width=\"8\" height=\"11\">&nbsp;Les cycle des poussi\u00e8res, cycle de l&rsquo;eau et des nuages, cycle du CO2 <br><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/planeto.geol.u-psud.fr\/local\/cache-vignettes\/L8xH11\/puce-32883.gif\" alt=\"-\" width=\"8\" height=\"11\">&nbsp;Les pal\u00e9oclimats martiens<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong> 2- Interaction climat-g\u00e9ologie sur Mars<br><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/planeto.geol.u-psud.fr\/local\/cache-vignettes\/L8xH11\/puce-32883.gif\" alt=\"-\" width=\"8\" height=\"11\">&nbsp;<\/strong>Rappels de g\u00e9omorphologie<br><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/planeto.geol.u-psud.fr\/local\/cache-vignettes\/L8xH11\/puce-32883.gif\" alt=\"-\" width=\"8\" height=\"11\">&nbsp;La cryosph\u00e8re martienne \u00e0 travers le temps. Vall\u00e9es de d\u00e9b\u00e2cle, glaciers, ravines. <br><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/planeto.geol.u-psud.fr\/local\/cache-vignettes\/L8xH11\/puce-32883.gif\" alt=\"-\" width=\"8\" height=\"11\">&nbsp;L&rsquo;\u00e9rosion fluviale sur Mars primitif (et sur Titan): g\u00e9omorphologie, min\u00e9ralogie. <\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>3- Pluton<\/strong> : une petite Mars gel\u00e9e<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>4- Le climat de V\u00e9nus<br><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/planeto.geol.u-psud.fr\/local\/cache-vignettes\/L8xH11\/puce-32883.gif\" alt=\"-\" width=\"8\" height=\"11\">&nbsp;<\/strong>Effet de serre, dynamique atmosph\u00e9rique et superrotation<br><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/planeto.geol.u-psud.fr\/local\/cache-vignettes\/L8xH11\/puce-32883.gif\" alt=\"-\" width=\"8\" height=\"11\">&nbsp;Le cycle du souffre et les nuages <\/p>\n\n\n\n<p class=\"wp-block-paragraph\"> <strong>5- Le climat de Titan, <\/strong>lune de Saturne<strong><br><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/planeto.geol.u-psud.fr\/local\/cache-vignettes\/L8xH11\/puce-32883.gif\" alt=\"-\" width=\"8\" height=\"11\">&nbsp;<\/strong>Dynamique atmosph\u00e9rique et superrotation<br><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/planeto.geol.u-psud.fr\/local\/cache-vignettes\/L8xH11\/puce-32883.gif\" alt=\"-\" width=\"8\" height=\"11\">&nbsp;Le cycle des hydrocarbures: brumes, nuages, et lacs  <\/p>\n\n\n\n<p class=\"wp-block-paragraph\"> <strong>6- Les atmosph\u00e8res des plan\u00e8tes g\u00e9antes<\/strong> : Jupiter, Saturne, Uranus, Neptune<strong><br><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/planeto.geol.u-psud.fr\/local\/cache-vignettes\/L8xH11\/puce-32883.gif\" alt=\"-\" width=\"8\" height=\"11\">&nbsp;<\/strong>Structures thermique, nuages et chimie atmosph\u00e9rique<br><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/planeto.geol.u-psud.fr\/local\/cache-vignettes\/L8xH11\/puce-32883.gif\" alt=\"-\" width=\"8\" height=\"11\">&nbsp;Dynamiques atmosph\u00e9rique<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Responsable&nbsp;:<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Fran\u00e7ois Forget, Laboratoire de M\u00e9t\u00e9orologie Dynamique, IPSL\/CNRS, Universit\u00e9 Pierre et Marie Curie, Tel&nbsp;: +33 6 71 20 07 50 &#8211; E-mail&nbsp;: forget[@robas]lmd.ipsl.fr<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/www.master-planeto.universite-paris-saclay.fr\/wp-content\/uploads\/2022\/02\/image4web_m2.jpg\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"302\" src=\"https:\/\/www.master-planeto.universite-paris-saclay.fr\/wp-content\/uploads\/2022\/02\/image4web_m2-1024x302.jpg\" alt=\"\" class=\"wp-image-619\" srcset=\"https:\/\/www.master-planeto.universite-paris-saclay.fr\/wp-content\/uploads\/2022\/02\/image4web_m2-1024x302.jpg 1024w, https:\/\/www.master-planeto.universite-paris-saclay.fr\/wp-content\/uploads\/2022\/02\/image4web_m2-300x89.jpg 300w, https:\/\/www.master-planeto.universite-paris-saclay.fr\/wp-content\/uploads\/2022\/02\/image4web_m2-768x227.jpg 768w, https:\/\/www.master-planeto.universite-paris-saclay.fr\/wp-content\/uploads\/2022\/02\/image4web_m2.jpg 1280w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>Ce module interdisciplinaire (climatologie\/g\u00e9ologie) a pour objectif de pr\u00e9senter les environnements et les atmosph\u00e8res sur diff\u00e9rents mondes du syst\u00e8me solaire et de d\u00e9crire les processus physiques qui contr\u00f4lent les climats et comment ils fa\u00e7onnent les surfaces plan\u00e9taires . Cela permet d&rsquo;illustrer des concepts th\u00e9oriques par des exemple observ\u00e9s, tout en restant au plus pr\u00e8s des &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/www.master-planeto.universite-paris-saclay.fr\/?page_id=85\" class=\"more-link\">Lire la suite de<span class=\"screen-reader-text\">\u00ab\u00a0UE 10 &#8211; Syst\u00e8mes climatiques et \u00e9volution des surfaces plan\u00e9taires\u00a0\u00bb<\/span><\/a><\/p>\n","protected":false},"author":11,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"inspiro_hide_title":false,"inspiro_hide_featured_image":false,"footnotes":""},"class_list":["post-85","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.master-planeto.universite-paris-saclay.fr\/index.php?rest_route=\/wp\/v2\/pages\/85","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.master-planeto.universite-paris-saclay.fr\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.master-planeto.universite-paris-saclay.fr\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.master-planeto.universite-paris-saclay.fr\/index.php?rest_route=\/wp\/v2\/users\/11"}],"replies":[{"embeddable":true,"href":"https:\/\/www.master-planeto.universite-paris-saclay.fr\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=85"}],"version-history":[{"count":7,"href":"https:\/\/www.master-planeto.universite-paris-saclay.fr\/index.php?rest_route=\/wp\/v2\/pages\/85\/revisions"}],"predecessor-version":[{"id":633,"href":"https:\/\/www.master-planeto.universite-paris-saclay.fr\/index.php?rest_route=\/wp\/v2\/pages\/85\/revisions\/633"}],"wp:attachment":[{"href":"https:\/\/www.master-planeto.universite-paris-saclay.fr\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=85"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}