{"id":101879,"date":"2026-07-12T13:48:40","date_gmt":"2026-07-12T11:48:40","guid":{"rendered":""},"modified":"2026-08-12T03:53:48","modified_gmt":"2026-08-12T01:53:48","slug":"019938be92f9-cea5d505-fbea-46ae-a55b-3612c5489c6c","status":"publish","type":"nva_publication","link":"https:\/\/nilu.gnist.dev\/en\/publications\/019938be92f9-cea5d505-fbea-46ae-a55b-3612c5489c6c\/","title":{"rendered":"METEOROLOGISKE DATA FRA NEDRE TELEMARK VINTEREN 1981\/82"},"content":{"rendered":"<p class=\"wp-block-paragraph\">En statistisk bearbeiding av meteorologiske data fra nedre Telemark i perioden 1.12.81-28.2.82 viser dominerende nordvestlige vinder, stabile tilfeller i mer enn 50% av tiden og en usedvanlig kald desember og januar m\u00e5ned.<\/p>\n","protected":false},"template":"","meta":{"_acf_changed":false,"_searchwp_excluded":"","_id":"","_status":"PUBLISHED","_sync_date":"2026-07-12 13:48:40","footnotes":""},"nva_tax_category":[1055],"class_list":["post-101879","nva_publication","type-nva_publication","status-publish","hentry","nva_tax_category-report"],"acf":[],"_links":{"self":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/101879","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\/101879\/revisions"}],"predecessor-version":[{"id":101880,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/101879\/revisions\/101880"}],"wp:attachment":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/media?parent=101879"}],"wp:term":[{"taxonomy":"nva_tax_category","embeddable":true,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_tax_category?post=101879"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}