{"id":135,"date":"2025-01-17T12:14:35","date_gmt":"2025-01-16T23:14:35","guid":{"rendered":"https:\/\/blogs.otago.ac.nz\/atmosphere\/?p=135"},"modified":"2025-01-17T12:14:35","modified_gmt":"2025-01-16T23:14:35","slug":"new-paper-in-nature-communications","status":"publish","type":"post","link":"https:\/\/blogs.otago.ac.nz\/atmosphere\/new-paper-in-nature-communications\/","title":{"rendered":"New paper in Nature Communications"},"content":{"rendered":"<p>Annika&#8217;s work explaining the physical mechanism from high altitude ozone loss to surface climate variability is now out: Sepp\u00e4l\u00e4, A., Kalakoski, N., Verronen, P.T. <i>et al.<\/i> Polar mesospheric ozone loss initiates downward coupling of solar signal in the Northern Hemisphere. <i>Nat Commun<\/i> <b>16<\/b>, 748 (2025). <a href=\"https:\/\/doi.org\/10.1038\/s41467-025-55966-z\">https:\/\/doi.org\/10.1038\/s41467-025-55966-z<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Annika&#8217;s work explaining the physical mechanism from high altitude ozone loss to surface climate variability is now out: Sepp\u00e4l\u00e4, A., Kalakoski, N., Verronen, P.T. et al. Polar mesospheric ozone loss initiates downward coupling of solar signal in the Northern Hemisphere. Nat Commun 16, 748 (2025). https:\/\/doi.org\/10.1038\/s41467-025-55966-z<\/p>\n","protected":false},"author":44922,"featured_media":0,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[111],"tags":[],"class_list":["post-135","post","type-post","status-publish","format-standard","hentry","category-news"],"_links":{"self":[{"href":"https:\/\/blogs.otago.ac.nz\/atmosphere\/wp-json\/wp\/v2\/posts\/135","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.otago.ac.nz\/atmosphere\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blogs.otago.ac.nz\/atmosphere\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.otago.ac.nz\/atmosphere\/wp-json\/wp\/v2\/users\/44922"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.otago.ac.nz\/atmosphere\/wp-json\/wp\/v2\/comments?post=135"}],"version-history":[{"count":0,"href":"https:\/\/blogs.otago.ac.nz\/atmosphere\/wp-json\/wp\/v2\/posts\/135\/revisions"}],"wp:attachment":[{"href":"https:\/\/blogs.otago.ac.nz\/atmosphere\/wp-json\/wp\/v2\/media?parent=135"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.otago.ac.nz\/atmosphere\/wp-json\/wp\/v2\/categories?post=135"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.otago.ac.nz\/atmosphere\/wp-json\/wp\/v2\/tags?post=135"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}