{"id":2289,"date":"2024-04-29T22:11:01","date_gmt":"2024-04-29T21:11:01","guid":{"rendered":"https:\/\/www.eurosolarnl.nl\/2024\/04\/29\/poleward-intensification-of-midlatitude-extreme-winds-under-warmer-climate\/"},"modified":"2024-04-29T22:11:01","modified_gmt":"2024-04-29T21:11:01","slug":"poleward-intensification-of-midlatitude-extreme-winds-under-warmer-climate","status":"publish","type":"post","link":"https:\/\/www.eurosolarnl.nl\/en_gb\/2024\/04\/29\/poleward-intensification-of-midlatitude-extreme-winds-under-warmer-climate\/","title":{"rendered":"Poleward intensification of midlatitude extreme winds under warmer climate"},"content":{"rendered":"<p>Modeling suggests that, under a warming climate, extreme near-surface wind speeds will increase by up to 3 percent towards the poles while decreasing by a similar amount in the lower midlatitudes.\u00a0<\/p>\n<p>\u200b<a href=\"https:\/\/www.climate.gov\/news-features\/feed\/poleward-intensification-midlatitude-extreme-winds-under-warmer-climate\" target=\"_blank\" class=\"feedzy-rss-link-icon\" rel=\"noopener\">Read More<\/a>\u00a0Modeling suggests that, under a warming climate, extreme near-surface wind speeds will increase by up to 3 percent towards the poles while decreasing by a similar amount in the lower midlatitudes.\u00a0\u00a0<\/p>","protected":false},"excerpt":{"rendered":"<p>Modeling suggests that, under a warming climate, extreme near-surface wind speeds will increase by up to 3 percent towards the poles while decreasing by a similar amount in the lower midlatitudes.\u00a0 \u200bRead More\u00a0Modeling suggests that, under a warming climate, extreme near-surface wind speeds will increase by up to 3 percent towards the poles while decreasing&#8230;<\/p>\n<p class=\"more-link-wrap\"><a href=\"https:\/\/www.eurosolarnl.nl\/en_gb\/2024\/04\/29\/poleward-intensification-of-midlatitude-extreme-winds-under-warmer-climate\/\" class=\"more-link\">Read More<span class=\"screen-reader-text\"> &ldquo;Poleward intensification of midlatitude extreme winds under warmer climate&rdquo;<\/span> &raquo;<\/a><\/p>\n","protected":false},"author":0,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_oct_exclude_from_cache":false,"footnotes":""},"categories":[50],"tags":[],"class_list":["post-2289","post","type-post","status-publish","format-standard","hentry","category-news"],"rttpg_featured_image_url":null,"rttpg_author":{"display_name":"","author_link":"https:\/\/www.eurosolarnl.nl\/en_gb\/author\/"},"rttpg_comment":0,"rttpg_category":"<a href=\"https:\/\/www.eurosolarnl.nl\/en_gb\/category\/news\/\" rel=\"category tag\">News<\/a>","rttpg_excerpt":"Modeling suggests that, under a warming climate, extreme near-surface wind speeds will increase by up to 3 percent towards the poles while decreasing by a similar amount in the lower midlatitudes.\u00a0 \u200bRead More\u00a0Modeling suggests that, under a warming climate, extreme near-surface wind speeds will increase by up to 3 percent towards the poles while decreasing...Read&hellip;","_links":{"self":[{"href":"https:\/\/www.eurosolarnl.nl\/en_gb\/wp-json\/wp\/v2\/posts\/2289","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.eurosolarnl.nl\/en_gb\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.eurosolarnl.nl\/en_gb\/wp-json\/wp\/v2\/types\/post"}],"replies":[{"embeddable":true,"href":"https:\/\/www.eurosolarnl.nl\/en_gb\/wp-json\/wp\/v2\/comments?post=2289"}],"version-history":[{"count":0,"href":"https:\/\/www.eurosolarnl.nl\/en_gb\/wp-json\/wp\/v2\/posts\/2289\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.eurosolarnl.nl\/en_gb\/wp-json\/wp\/v2\/media?parent=2289"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.eurosolarnl.nl\/en_gb\/wp-json\/wp\/v2\/categories?post=2289"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.eurosolarnl.nl\/en_gb\/wp-json\/wp\/v2\/tags?post=2289"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}