{"id":90294,"date":"2026-06-26T13:12:58","date_gmt":"2026-06-26T11:12:58","guid":{"rendered":""},"modified":"2026-06-26T13:27:00","modified_gmt":"2026-06-26T11:27:00","slug":"0198cc4f251f-fb8a487c-45f3-4506-88be-e8557e31d651","status":"publish","type":"nva_publication","link":"https:\/\/nilu.gnist.dev\/en\/publications\/0198cc4f251f-fb8a487c-45f3-4506-88be-e8557e31d651\/","title":{"rendered":"Duration and decay of extreme vortex events in the polar stratosphere: Comparison of the ECMWF Seasonal Forecast Model with reanalyses"},"content":{"rendered":"","protected":false},"template":"","meta":{"_acf_changed":false,"_searchwp_excluded":"","_id":"","_status":"PUBLISHED","_sync_date":"2026-06-26 13:12:58","footnotes":""},"nva_tax_category":[985],"class_list":["post-90294","nva_publication","type-nva_publication","status-publish","hentry","nva_tax_category-poster"],"acf":[],"_links":{"self":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/90294","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication"}],"about":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/types\/nva_publication"}],"version-history":[{"count":1,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/90294\/revisions"}],"predecessor-version":[{"id":90295,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/90294\/revisions\/90295"}],"wp:attachment":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/media?parent=90294"}],"wp:term":[{"taxonomy":"nva_tax_category","embeddable":true,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_tax_category?post=90294"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}