{"id":375,"date":"2006-11-26T19:07:54","date_gmt":"2006-11-27T00:07:54","guid":{"rendered":"\/?p=375"},"modified":"2012-01-15T16:11:52","modified_gmt":"2012-01-15T21:11:52","slug":"the-sky-is-falling","status":"publish","type":"post","link":"https:\/\/www.realclimate.org\/index.php\/archives\/2006\/11\/the-sky-is-falling\/","title":{"rendered":"The sky IS falling <lang_fr>Le ciel nous tombe vraiment sur la t\u00eate<\/lang_fr>"},"content":{"rendered":"<div class=\"kcite-section\" kcite-section-id=\"375\">\n<p><a href=\"http:\/\/www.sciencemag.org\/cgi\/content\/full\/314\/5803\/1253\" target=\"_blank\"><img decoding=\"async\" data-src=\"\/images\/skyfalling.gif\" width=40% align=\"right\" src=\"data:image\/svg+xml;base64,PHN2ZyB3aWR0aD0iMSIgaGVpZ2h0PSIxIiB4bWxucz0iaHR0cDovL3d3dy53My5vcmcvMjAwMC9zdmciPjwvc3ZnPg==\" class=\"lazyload\" style=\"--smush-placeholder-width: 348px; --smush-placeholder-aspect-ratio: 348\/383;\" \/><\/a><br \/>\nA timely perspective article in <em>Science<\/em> this week addresses the issues of upper atmosphere change. &#8216;Upper&#8217; atmosphere here is the stratosphere up to the ionosphere (~20 to 300 km). <a href=\"http:\/\/www.sciencemag.org\/cgi\/content\/full\/314\/5803\/1253\">La\u0161tovi\u010dka et al<\/a> point out that cooling trends are exactly as predicted by increasing greenhouse gas trends, and that the increase in density that this implies is causing various ionspheric layers to &#8216;fall&#8217;. This was highlighted a few years back by <a href=\"http:\/\/www.agu.org\/pubs\/crossref\/1998\/98JA01629.shtml\">Jarvis et al (1998)<\/a> and in <a href=\"http:\/\/list.uvm.edu\/cgi-bin\/wa?A2=ind9905&#038;L=climateaction&#038;D=1&#038;T=0&#038;P=273\">New Scientist<\/a> in 1999 (and I apologise for stealing their headline!). <\/p>\n<p>The changes in the figure are related to the cooling seen in the lower stratospheric MSU-4 records (<a href=\"http:\/\/www.ghcc.msfc.nasa.gov\/MSU\/images\/strato_temp.gif\">UAH<\/a> or <a href=\"http:\/\/www.ssmi.com\/pub\/msu\/graphics\/plots\/sc_Rss_compare_TS_channel_tls.png\">RSS<\/a>), but the changes there (~ 15-20 km) are predominantly due to ozone depletion. The higher up one goes, the more important the CO<sub>2<\/sub> related cooling is. It&#8217;s interesting to note that significant solar forcing would have exactly the opposite effect (it would cause a warming) &#8211; yet another reason to doubt that solar forcing is a significant factor in recent decades.<\/p>\n<p><strong>Update:<\/strong> The best explanation for the cooling trends can be found on <a href=\"http:\/\/www.atmosphere.mpg.de\/enid\/20c.html\">ESPERE<\/a> (<a href=\"http:\/\/www.xplora.org\/downloads\/Knoppix\/ESPERE\/ESPEREdez05\/ESPEREde\/www.atmosphere.mpg.de\/enid\/0,55a304092d09\/2__Ozone\/-_Cooling_nd.html\">alternative site<\/a>), in particular, <a href=\"http:\/\/www.atmosphere.mpg.de\/media\/archive\/1461.jpg\">figure 3<\/a> (<a href=\"http:\/\/www.realclimate.org\/images\/\/clough_iacono.jpg\">alt. version<\/a>).<\/p>\n<p><lang_fr><br \/>\n<small>Traduit par Etienne Pesnelle<\/small><br \/>\n<a href=\"http:\/\/www.sciencemag.org\/cgi\/content\/full\/314\/5803\/1253\" target=\"_blank\"><img decoding=\"async\" data-src=\"\/images\/skyfalling.gif\" width=40% align=\"right\" src=\"data:image\/svg+xml;base64,PHN2ZyB3aWR0aD0iMSIgaGVpZ2h0PSIxIiB4bWxucz0iaHR0cDovL3d3dy53My5vcmcvMjAwMC9zdmciPjwvc3ZnPg==\" class=\"lazyload\" style=\"--smush-placeholder-width: 348px; --smush-placeholder-aspect-ratio: 348\/383;\" \/><\/a>Dans le num\u00e9ro de cette semaine de Science, un article opportun de mise en perspective traite des probl\u00e8mes du changement de l&#8217;atmosph\u00e8re sup\u00e9rieure. Ladite atmosph\u00e8re &#8220;sup\u00e9rieure&#8221; consiste en la stratosph\u00e8re jusqu&#8217;\u00e0 l&#8217;ionosph\u00e8re (~20 \u00e0 300 km). <a href=\"http:\/\/www.sciencemag.org\/cgi\/content\/full\/314\/5803\/1253\">La\u0161tovicka et al<\/a> soulignent que la tendance au refroidissement est exactement telle que pr\u00e9dite par la tendance \u00e0 la hausse des gaz \u00e0 effet de serre, et que l&#8217;accroissement de densit\u00e9 que cela implique est en train de provoquer la &#8220;chute&#8221; de diff\u00e9rentes couches de la ionosph\u00e8re. Cela a \u00e9t\u00e9 mis en exergue il y a quelques ann\u00e9es par <a href=\"http:\/\/www.agu.org\/pubs\/crossref\/1998\/98JA01629.shtml\">Jarvis et al.<\/a> (1998) et dans <a href=\"http:\/\/list.uvm.edu\/cgi-bin\/wa?A2=ind9905&#038;L=climateaction&#038;D=1&#038;T=0&#038;P=273\">New Scientist<\/a> en 1999 (et je m&#8217;excuse de leur avoir vol\u00e9 le titre de leur article!).<\/p>\n<p>Les changements dans le graphique sont li\u00e9s au refroidissement constat\u00e9 dans les enregistrements MSU-4 de la basse stratosph\u00e8re (que ce soit ceux provenant des bases de donn\u00e9es <a href=\"http:\/\/www.ghcc.msfc.nasa.gov\/MSU\/images\/strato_temp.gif\">UAH<\/a> ou <a href=\"http:\/\/www.ssmi.com\/pub\/msu\/graphics\/plots\/sc_Rss_compare_TS_channel_tls.png\">RSS<\/a>), mais les changements \u00e0 ces altitudes (~ 15-20 km) sont principalement d\u00fbs \u00e0 la rar\u00e9faction de l&#8217;ozone. Plus on monte, plus le refroidissement d\u00fb au CO<sub>2<\/sub> est important. Il est int\u00e9ressant de noter qu&#8217;un for\u00e7age solaire significatif aurait exactement l&#8217;effet inverse (il provoquerait un r\u00e9chauffement) &#8211; encore une autre raison de douter que le for\u00e7age solaire est un facteur significatif [du r\u00e9chauffement climatique] des derni\u00e8res d\u00e9cennies.<\/p>\n<p><strong>Mise \u00e0 jour<\/strong> : la meilleure explication des tendances au refroidissement peut \u00eatre trouv\u00e9e sur <a href=\"http:\/\/www.atmosphere.mpg.de\/enid\/20c.html\">ESPERE<\/a>, en particulier la <a href=\"http:\/\/www.atmosphere.mpg.de\/media\/archive\/1461.jpg\">figure 3<\/a>.<\/lang_fr><\/p>\n<!-- kcite active, but no citations found -->\n<\/div> <!-- kcite-section 375 -->","protected":false},"excerpt":{"rendered":"<p>A timely perspective article in Science this week addresses the issues of upper atmosphere change. &#8216;Upper&#8217; atmosphere here is the stratosphere up to the ionosphere (~20 to 300 km). La\u0161tovi\u010dka et al point out that cooling trends are exactly as predicted by increasing greenhouse gas trends, and that the increase in density that this implies [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_exactmetrics_skip_tracking":false,"_exactmetrics_sitenote_active":false,"_exactmetrics_sitenote_note":"","_exactmetrics_sitenote_category":0,"_genesis_hide_title":false,"_genesis_hide_breadcrumbs":false,"_genesis_hide_singular_image":false,"_genesis_hide_footer_widgets":false,"_genesis_custom_body_class":"","_genesis_custom_post_class":"","_genesis_layout":"","footnotes":""},"categories":[1,3,26],"tags":[],"class_list":["post-375","post","type-post","status-publish","format-standard","category-climate-science","category-greenhouse-gases","category-rc-forum","entry"],"aioseo_notices":[],"aioseo_head":"\n\t\t<!-- All in One SEO 4.9.9 - aioseo.com -->\n\t<meta name=\"description\" content=\"RealClimate: A timely perspective article in Science this week addresses the issues of upper atmosphere change. &#039;Upper&#039; atmosphere here is the stratosphere up to the ionosphere (~20 to 300 km). 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