{"id":98749,"date":"2026-07-08T15:00:46","date_gmt":"2026-07-08T13:00:46","guid":{"rendered":""},"modified":"2026-07-12T20:54:48","modified_gmt":"2026-07-12T18:54:48","slug":"019938961231-011493c7-1e48-4f59-b7fc-fd7d45f0c17d","status":"publish","type":"nva_publication","link":"https:\/\/nilu.gnist.dev\/en\/publications\/019938961231-011493c7-1e48-4f59-b7fc-fd7d45f0c17d\/","title":{"rendered":"VIND OG STABILITETSFORHOLD I H\u00d8YANGER I PERIODEN OKTOBER 1977 &#8211; OKTOBER 1978."},"content":{"rendered":"<p class=\"wp-block-paragraph\">Vind, temperatur og relativ fuktighet er registrert i H\u00f8yanger hver time i et \u00e5r. Dataene er bearbeidet med sikte p\u00e5 \u00e5 belyse spredningsforholdene. Representativiteten av m\u00e5leperiodene er vurdert ved hjelp av data fra n\u00e6rliggende klimastasjoner.<\/p>\n","protected":false},"template":"","meta":{"_acf_changed":false,"_searchwp_excluded":"","_id":"","_status":"PUBLISHED","_sync_date":"2026-07-08 15:00:46","footnotes":""},"nva_tax_category":[1055],"class_list":["post-98749","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\/98749","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\/98749\/revisions"}],"predecessor-version":[{"id":98750,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/98749\/revisions\/98750"}],"wp:attachment":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/media?parent=98749"}],"wp:term":[{"taxonomy":"nva_tax_category","embeddable":true,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_tax_category?post=98749"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}