{"id":809,"date":"2020-12-08T11:59:24","date_gmt":"2020-12-08T15:59:24","guid":{"rendered":"https:\/\/storm.uml.edu\/~metweb\/Blog\/?p=809"},"modified":"2021-09-16T16:39:07","modified_gmt":"2021-09-16T16:39:07","slug":"record-global-temperatures-for-november-2020","status":"publish","type":"post","link":"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/2020\/12\/08\/record-global-temperatures-for-november-2020\/","title":{"rendered":"Record Global Temperatures for November 2020"},"content":{"rendered":"\n<p>by Dr. Mathew Barlow, UML Professor of Climate Science<\/p>\n\n\n\n<p>Globally, November 2020 was the warmest November on record:  <a href=\"https:\/\/climate.copernicus.eu\/surface-air-temperature-november-2020\">https:\/\/climate.copernicus.eu\/surface-air-temperature-november-2020<\/a><\/p>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"2500\" height=\"1083\" src=\"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/map_1month_anomaly_Global_ea_2t_202011_v02.png\" alt=\"\" class=\"wp-image-811\" srcset=\"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/map_1month_anomaly_Global_ea_2t_202011_v02.png 2500w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/map_1month_anomaly_Global_ea_2t_202011_v02-300x130.png 300w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/map_1month_anomaly_Global_ea_2t_202011_v02-1024x444.png 1024w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/map_1month_anomaly_Global_ea_2t_202011_v02-768x333.png 768w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/map_1month_anomaly_Global_ea_2t_202011_v02-1536x665.png 1536w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/map_1month_anomaly_Global_ea_2t_202011_v02-2048x887.png 2048w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/map_1month_anomaly_Global_ea_2t_202011_v02-1568x679.png 1568w\" sizes=\"auto, (max-width: 767px) 89vw, (max-width: 1000px) 54vw, (max-width: 1071px) 543px, 580px\" \/><\/figure><\/div>\n\n\n\n<p>The reds indicate temperatures warmer than the 1981-2010 average and the blues indicate temperatures colder than the 1981-2010 average. (The 1981-2010 period is the current international reference period.) You&#8217;ll notice a lot of red.<\/p>\n\n\n\n<p>While temperatures for any specific location and any particular month are strongly influenced by weather and natural climate variability, the fact that the map shows mostly warmer-than-average temperatures is due to human-caused climate change.  <\/p>\n\n\n\n<p>Of the globally-averaged warming that&#8217;s occurred over the last 150 years, roughly how much has been caused by humans? <strong>All of it<\/strong>: <a href=\"https:\/\/www.carbonbrief.org\/analysis-why-scientists-think-100-of-global-warming-is-due-to-humans\">https:\/\/www.carbonbrief.org\/analysis-why-scientists-think-100-of-global-warming-is-due-to-humans<\/a><\/p>\n\n\n\n<p>You probably noticed that the largest temperature differences are in the Arctic region &#8211; this is known as &#8220;Arctic Amplification.&#8221; Here it is highlighted in a 3D perspective animation:<\/p>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1476\" height=\"1058\" src=\"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/nov_2020_2.gif\" alt=\"\" class=\"wp-image-812\"\/><figcaption>Animation by M. Barlow<\/figcaption><\/figure><\/div>\n\n\n\n<p>That animation uses a slightly different dataset and reference period from the first figure but shows the same overall picture.  The 3D perspective is inspired by Greg Fiske&#8217;s excellent graphic of projected temperatures, which show similar features:<\/p>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large is-resized\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/EgcVhRxXYAAWaKJ.jpeg\" alt=\"\" class=\"wp-image-813\" width=\"280\" height=\"401\" srcset=\"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/EgcVhRxXYAAWaKJ.jpeg 1785w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/EgcVhRxXYAAWaKJ-209x300.jpeg 209w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/EgcVhRxXYAAWaKJ-714x1024.jpeg 714w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/EgcVhRxXYAAWaKJ-768x1101.jpeg 768w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/EgcVhRxXYAAWaKJ-1071x1536.jpeg 1071w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/EgcVhRxXYAAWaKJ-1428x2048.jpeg 1428w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/EgcVhRxXYAAWaKJ-1568x2249.jpeg 1568w\" sizes=\"auto, (max-width: 280px) 100vw, 280px\" \/><figcaption>Image by Greg Fiske, RCP 8.5 scenario<\/figcaption><\/figure><\/div>\n\n\n\n<p>The projection shown is for mid-century temperature increases relative to 1880-1920, based on RCP 8.5 emissions: <a href=\"https:\/\/twitter.com\/WoodwellClimate\/status\/1299030866988019712\">https:\/\/twitter.com\/WoodwellClimate\/status\/1299030866988019712<\/a><\/p>\n\n\n\n<p>Arctic Amplification is a robust feature of both observed and projected temperature changes. The causes are an area of active research and involve a number of different factors.  There&#8217;s a nice summary of the current state of understanding in Box 3.1 of the IPCC SROCC report: <a href=\"https:\/\/www.ipcc.ch\/srocc\/chapter\/chapter-3-2\/\">https:\/\/www.ipcc.ch\/srocc\/chapter\/chapter-3-2\/<\/a><\/p>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large is-resized\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/Screen-Shot-2020-12-08-at-10.36.53-AM.png\" alt=\"\" class=\"wp-image-815\" width=\"483\" height=\"397\" srcset=\"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/Screen-Shot-2020-12-08-at-10.36.53-AM.png 1262w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/Screen-Shot-2020-12-08-at-10.36.53-AM-300x247.png 300w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/Screen-Shot-2020-12-08-at-10.36.53-AM-1024x842.png 1024w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/Screen-Shot-2020-12-08-at-10.36.53-AM-768x632.png 768w\" sizes=\"auto, (max-width: 483px) 100vw, 483px\" \/><figcaption>From SROCC, Chapter 3, Box 3.1<\/figcaption><\/figure><\/div>\n\n\n\n<p>You may also have noticed the colder-than-average temperatures in the tropical Pacific. Those are associated with the &#8220;La Ni\u00f1a&#8221; phenomenon, the opposite phase of El Ni\u00f1o; both of which are naturally-occurring.  La Ni\u00f1a has characteristic global impacts; for instance, on rainfall:<\/p>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"2700\" height=\"1722\" src=\"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/LaNinaandRainfall-2.png\" alt=\"\" class=\"wp-image-814\" srcset=\"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/LaNinaandRainfall-2.png 2700w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/LaNinaandRainfall-2-300x191.png 300w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/LaNinaandRainfall-2-1024x653.png 1024w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/LaNinaandRainfall-2-768x490.png 768w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/LaNinaandRainfall-2-1536x980.png 1536w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/LaNinaandRainfall-2-2048x1306.png 2048w, https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-content\/uploads\/2020\/12\/LaNinaandRainfall-2-1568x1000.png 1568w\" sizes=\"auto, (max-width: 767px) 89vw, (max-width: 1000px) 54vw, (max-width: 1071px) 543px, 580px\" \/><\/figure><\/div>\n\n\n\n<p>More information on the current state and forecasts for La Nina is available at: <a href=\"https:\/\/iridl.ldeo.columbia.edu\/maproom\/IFRC\/FIC\/laninarain.html\">https:\/\/iridl.ldeo.columbia.edu\/maproom\/IFRC\/FIC\/laninarain.html<\/a><\/p>\n\n\n\n<p>For more information on our department at UMASS Lowell, please see <a href=\"https:\/\/www.uml.edu\/sciences\/eeas\/\">https:\/\/www.uml.edu\/sciences\/eeas\/<\/a> and for more information on the campus&#8217; climate change-related activities, please see <a href=\"https:\/\/climatechangeinitiative.org\">https:\/\/climatechangeinitiative.org<\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>by Dr. Mathew Barlow, UML Professor of Climate Science Globally, November 2020 was the warmest November on record: https:\/\/climate.copernicus.eu\/surface-air-temperature-november-2020 The reds indicate temperatures warmer than the 1981-2010 average and the blues indicate temperatures colder than the 1981-2010 average. (The 1981-2010 period is the current international reference period.) You&#8217;ll notice a lot of red. While temperatures [&hellip;]<\/p>\n","protected":false},"author":5,"featured_media":812,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[2,3,5,6,12,1],"tags":[],"class_list":["post-809","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-arctic","category-autumn","category-climate-change","category-climatology","category-heat","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-json\/wp\/v2\/posts\/809","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-json\/wp\/v2\/users\/5"}],"replies":[{"embeddable":true,"href":"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-json\/wp\/v2\/comments?post=809"}],"version-history":[{"count":1,"href":"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-json\/wp\/v2\/posts\/809\/revisions"}],"predecessor-version":[{"id":948,"href":"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-json\/wp\/v2\/posts\/809\/revisions\/948"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-json\/wp\/v2\/media\/812"}],"wp:attachment":[{"href":"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-json\/wp\/v2\/media?parent=809"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-json\/wp\/v2\/categories?post=809"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/storm.uml.edu\/~metweb\/newBlog\/wordpress\/wp-json\/wp\/v2\/tags?post=809"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}