{"id":121489,"date":"2026-09-11T21:53:58","date_gmt":"2026-09-11T19:53:58","guid":{"rendered":"https:\/\/nilu.gnist.dev\/publikasjoner\/sodar-malinger-i-oslo-vinteren-1986-87\/"},"modified":"2026-09-11T21:53:58","modified_gmt":"2026-09-11T19:53:58","slug":"sodar-malinger-i-oslo-vinteren-1986-87","status":"publish","type":"nva_publication","link":"https:\/\/nilu.gnist.dev\/en\/publications\/sodar-malinger-i-oslo-vinteren-1986-87\/","title":{"rendered":"SODAR m\u00e5linger i Oslo, vinteren 1986\/87."},"content":{"rendered":"<p class=\"wp-block-paragraph\">Vindfeltet over sentrum i Oslo ble m\u00e5lt ved hjelp av vet akustisk instrument (SODAR). De innsamlede data gir god informasjon om luftbevegelsen opp til 200 m h\u00f8yde over bakken. Over 200 m h\u00f8yde er informasjonsmengden liten. Hyppige sjiktninger ble funnet i 100 m og 200 m h\u00f8yde. Bygnings- og gatestruktur influerer luftbevegelsen opp til 100 m over bakken.<\/p>\n","protected":false},"template":"","meta":{"_acf_changed":false,"_searchwp_excluded":"","_id":"","_status":"PUBLISHED","_sync_date":"2026-09-11 15:06:21","footnotes":""},"nva_tax_category":[1095],"class_list":["post-121489","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\/121489","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":0,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/121489\/revisions"}],"wp:attachment":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/media?parent=121489"}],"wp:term":[{"taxonomy":"nva_tax_category","embeddable":true,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_tax_category?post=121489"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}