{"id":19117,"date":"2025-06-04T07:59:12","date_gmt":"2025-06-04T08:59:12","guid":{"rendered":"https:\/\/govmin.gl\/?p=19117"},"modified":"2025-06-03T15:28:05","modified_gmt":"2025-06-03T16:28:05","slug":"situationsvurdering-fra-onsdag-den-4-juni-2025","status":"publish","type":"post","link":"https:\/\/govmin.gl\/da\/2025\/06\/situationsvurdering-fra-onsdag-den-4-juni-2025\/","title":{"rendered":"Situationsvurdering fra onsdag den 4. juni 2025"},"content":{"rendered":"

Overv\u00e5gningen viser ingen risiko for st\u00f8rre, n\u00e6rt forest\u00e5ende fjeldskred eller farlige b\u00f8lgeopskyl i beboede omr\u00e5der.<\/strong><\/p>\n

Spontane skred af mindre omfang kan forekomme p\u00e5 fjeldskr\u00e5ningerne markeret med r\u00f8dt i figur 1 og 2. Ophold frar\u00e5des n\u00e6r omr\u00e5derne markeret med r\u00f8dt, b\u00e5de til lands og p\u00e5 havet.<\/strong><\/p>\n

Opsummering af overv\u00e5gningsdata for den seneste m\u00e5ned<\/strong><\/p>\n

Umiammakku Nunaat:<\/u>
\nOverv\u00e5gningsdata viser fortsat aktivitet i de overv\u00e5gede fjeldpartier ved Umiammakku Nunaat.<\/p>\n

Der observeres stenfald og stenskred samt relativt langsomme, konstante bev\u00e6gelser i dele af fjeldsiderne. Dette er i tr\u00e5d med aktiviteten observeret i foreg\u00e5ende m\u00e5neder (se figur 1).<\/p>\n

Vejrstationen i Umiammakku Nunaat har registreret temperaturer svingende mellem -13 \u00b0C og +10 \u00b0C. Dage med temperaturer over frysepunktet har haft hyppigere stenskred sammenlignet med dage med frost. Det forventes, at bev\u00e6gelserne i fjeldsiderne vil stige gennem sommeren.<\/p>\n

Kangerluarsuk:<\/u>
\nGPS-stationerne ved \u201cKangerluarsuk Kangilleq\u201d viser en let acceleration i bev\u00e6gelserne registreret den seneste m\u00e5ned, hvilket er svarende til tidligere \u00e5rs observationer i overgangen fra for\u00e5r til sommer.<\/p>\n

I den kystn\u00e6re del af skr\u00e5ningen, ved \u201cKangerluarsuk Killeq\u201d, registreres fortsat konstante forskydninger og hyppige stenskred (se figur 2). Det kan ikke udelukkes, at en samlet massebev\u00e6gelse vil skride ud i fjorden fra omr\u00e5det. En s\u00e5dan h\u00e6ndelse vurderes dog ikke at udg\u00f8re en risiko for beboede omr\u00e5der, men kan potentielt medf\u00f8re lokale opskyl i Kangerluarsuk-omr\u00e5det.<\/p>\n

Registrerede stenskred og bev\u00e6gelser i de overv\u00e5gede fjeldskr\u00e5ninger er vist som farvede omr\u00e5der p\u00e5 figur 1 og 2 nedenfor. Bl\u00e5 omr\u00e5der angiver vedvarende glidende bev\u00e6gelse, mens r\u00f8de omr\u00e5der markerer lokaliteter med gentagne stenskred inden for den seneste m\u00e5ned.<\/p>\n

Den n\u00e6ste situationsvurdering vil blive offentliggjort onsdag den 2. juli 2025. I tilf\u00e6lde af kritiske \u00e6ndringer i de overv\u00e5gede omr\u00e5der vil en meddelelse offentligg\u00f8res tidligere.<\/p>\n

\"\"<\/a><\/p>\n

Figure 1. Oversigtskort over registrerede bev\u00e6gelser og stenskred i Umiammakku Nunaat i l\u00f8bet af maj 2025.<\/p>\n

\"\"<\/a>
Figure 2. Oversigtskort over registrerede bev\u00e6gelser og stenskred i Kangerluarsuk i l\u00f8bet af maj 2025. I den kystn\u00e6re del af skr\u00e5ningen, Kangerluarsuk Killeq, er aktiviteten fortsat stor, med hyppige stenfald og mindre skred.<\/figcaption><\/figure>\n","protected":false},"excerpt":{"rendered":"

Overv\u00e5gningen viser ingen risiko for st\u00f8rre, n\u00e6rt forest\u00e5ende fjeldskred eller farlige b\u00f8lgeopskyl i beboede omr\u00e5der. Spontane skred af mindre omfang kan forekomme p\u00e5 fjeldskr\u00e5ningerne markeret med r\u00f8dt i figur 1 og 2. Ophold frar\u00e5des n\u00e6r omr\u00e5derne markeret med r\u00f8dt, b\u00e5de til lands og p\u00e5 havet. Opsummering af overv\u00e5gningsdata for den seneste m\u00e5ned Umiammakku Nunaat: Overv\u00e5gningsdata […]<\/p>\n","protected":false},"author":43,"featured_media":19115,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","ast-disable-related-posts":"","theme-transparent-header-meta":"default","adv-header-id-meta":"","stick-header-meta":"default","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"set","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"iawp_total_views":85,"footnotes":""},"categories":[2118],"tags":[],"class_list":["post-19117","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-seneste-vurdering-af-overvaagede-omraader"],"_links":{"self":[{"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/posts\/19117","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/users\/43"}],"replies":[{"embeddable":true,"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/comments?post=19117"}],"version-history":[{"count":1,"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/posts\/19117\/revisions"}],"predecessor-version":[{"id":19119,"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/posts\/19117\/revisions\/19119"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/media\/19115"}],"wp:attachment":[{"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/media?parent=19117"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/categories?post=19117"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/tags?post=19117"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}