{"id":100845,"date":"2026-07-08T15:04:40","date_gmt":"2026-07-08T13:04:40","guid":{"rendered":""},"modified":"2026-07-13T09:42:11","modified_gmt":"2026-07-13T07:42:11","slug":"019938b7041d-aa18231e-4149-4c9e-b0e1-df1e1533d762","status":"publish","type":"nva_publication","link":"https:\/\/nilu.gnist.dev\/en\/publications\/019938b7041d-aa18231e-4149-4c9e-b0e1-df1e1533d762\/","title":{"rendered":"Overv\u00e5king av atmosf\u00e6rens ozonlag og naturlig ultrafiolett str\u00e5ling. \u00c5rsrapport 2000."},"content":{"rendered":"<p class=\"wp-block-paragraph\">Rapporten presenterer m\u00e5ledata for totalozon, vertikalfordelingen av ozon og UV-str\u00e5ling ved norske m\u00e5lestasjoner i2000. For Oslo og And\u00f8ya er trenden i totalozon for tidsrommet 1979 &#8211; 2000 beregnet<\/p>\n","protected":false},"template":"","meta":{"_acf_changed":false,"_searchwp_excluded":"","_id":"","_status":"PUBLISHED","_sync_date":"2026-07-08 15:05:49","footnotes":""},"nva_tax_category":[1055],"class_list":["post-100845","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\/100845","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\/100845\/revisions"}],"predecessor-version":[{"id":100846,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/100845\/revisions\/100846"}],"wp:attachment":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/media?parent=100845"}],"wp:term":[{"taxonomy":"nva_tax_category","embeddable":true,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_tax_category?post=100845"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}