{"id":18477,"date":"2024-10-02T07:30:00","date_gmt":"2024-10-02T08:30:00","guid":{"rendered":"https:\/\/govmin.gl\/?p=18477"},"modified":"2024-10-02T07:30:00","modified_gmt":"2024-10-02T08:30:00","slug":"situationsvurdering-fra-onsdag-den-2-oktober-2024","status":"publish","type":"post","link":"https:\/\/govmin.gl\/da\/2024\/10\/situationsvurdering-fra-onsdag-den-2-oktober-2024\/","title":{"rendered":"Situationsvurdering fra onsdag den 2. oktober 2024"},"content":{"rendered":"<p style=\"font-weight: 400;\"><strong>P\u00e5 baggrund af data fra den aktuelle overv\u00e5gning kan det oplyses, at der ikke ses en n\u00e6rt forest\u00e5ende fare for st\u00f8rre fjeldskred eller efterf\u00f8lgende farlige b\u00f8lgeopskyl ved beboede omr\u00e5der i Uummannaq Fjordsystemet. Der er fortsat stenfaldsaktivitet og sandsynlighed for mindre skredh\u00e6ndelser ved de ustabile fjeldskr\u00e5ninger kortlagt med r\u00f8d farve i figur 1 og 2. Omkring disse omr\u00e5der frar\u00e5des ophold t\u00e6t ved fjeldpartierne.<\/strong><strong>\u00a0<\/strong><\/p>\n<p style=\"font-weight: 400;\"><strong>Sammenfatning af overv\u00e5gningsdata opsamlet siden juli 2024<\/strong><\/p>\n<p style=\"font-weight: 400;\">De indsamlede overv\u00e5gningsdata siden begyndelsen af juli 2024 viser konstante forskydninger i varierende st\u00f8rrelsesordener af de ustabile fjeldpartier i Umiammakku Nunaat og Kangerluarsuk.<\/p>\n<p style=\"font-weight: 400;\">Observerede forskydninger i de overv\u00e5gede fjeldpartier vises som farvede omr\u00e5der p\u00e5 de nedenst\u00e5ende kort i figur 2 og 3: De bl\u00e5 omr\u00e5der markerer registrerede bev\u00e6gelser, mens de r\u00f8de farveomr\u00e5der angiver steder med flere stenfald og mindre skredh\u00e6ndelser siden begyndelsen af juli 2024.<\/p>\n<p style=\"font-weight: 400;\">B\u00e5de i Kangerluarsuk og Umiammakku Nunaat 3 har bev\u00e6gelseshastigheder v\u00e6ret let \u00f8gede i l\u00f8bet af de sene sommerm\u00e5neder og ligeledes har hyppigheden af stenfald i de nederste dele v\u00e6ret st\u00f8rre. Det samme forhold har v\u00e6ret g\u00e6ldende i sensommerperioden i 2023.<\/p>\n<p style=\"font-weight: 400;\">Fjeldskredsgruppens geologer har udf\u00f8rt feltarbejde i Umiammakku Nunaat og Kangerluarsuk i august 2024. Feltarbejdet har best\u00e5et af vedligeholdelse og opgradering af overv\u00e5gningssystemer, droneopm\u00e5linger samt seismiske unders\u00f8gelser i de ustabile fjeldpartier, og indledende regionale screeningsunders\u00f8gelser i Uummannaq fjordsystemet. Analyser af indsamlet data vil foreg\u00e5 i dette efter\u00e5r og i de kommende vinterm\u00e5neder.<\/p>\n<p style=\"font-weight: 400;\">N\u00e6ste situationsvurdering vil blive udgivet onsdag den 7. november 2024. Men hvis der sker kritiske \u00e6ndringer i de overv\u00e5gede fjeldsider, vil det blive meddelt tidligere.<\/p>\n<figure id=\"attachment_18471\" aria-describedby=\"caption-attachment-18471\" style=\"width: 1716px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede1.webp\"><img fetchpriority=\"high\" decoding=\"async\" class=\"wp-image-18470 size-full\" src=\"https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede1.webp\" alt=\"\" width=\"1716\" height=\"1216\" srcset=\"https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede1.webp 1716w, https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede1-300x213.webp 300w, https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede1-1024x726.webp 1024w, https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede1-768x544.webp 768w, https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede1-1536x1088.webp 1536w, https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede1-1320x935.webp 1320w\" sizes=\"(max-width: 1716px) 100vw, 1716px\" \/><\/a><figcaption id=\"caption-attachment-18471\" class=\"wp-caption-text\"><strong>Figur 2.<\/strong> Oversigtskort over registrerede bev\u00e6gelser og stenfald i Umiammakku Nunaat siden begyndelsen af juli 2024.<\/figcaption><\/figure>\n<figure id=\"attachment_18468\" aria-describedby=\"caption-attachment-18468\" style=\"width: 1716px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede2.webp\"><img decoding=\"async\" class=\"size-full wp-image-18467\" src=\"https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede2.webp\" alt=\"\" width=\"1716\" height=\"1216\" srcset=\"https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede2.webp 1716w, https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede2-300x213.webp 300w, https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede2-1024x726.webp 1024w, https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede2-768x544.webp 768w, https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede2-1536x1088.webp 1536w, https:\/\/govmin.gl\/wp-content\/uploads\/2024\/10\/Billede2-1320x935.webp 1320w\" sizes=\"(max-width: 1716px) 100vw, 1716px\" \/><\/a><figcaption id=\"caption-attachment-18468\" class=\"wp-caption-text\"><strong>Figur 2.<\/strong> Oversigtskort over registrerede bev\u00e6gelser og stenfald i Kangerluarsuk siden begyndelsen af juli 2024.<\/figcaption><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>P\u00e5 baggrund af data fra den aktuelle overv\u00e5gning kan det oplyses, at der ikke ses en n\u00e6rt forest\u00e5ende fare for st\u00f8rre fjeldskred eller efterf\u00f8lgende farlige b\u00f8lgeopskyl ved beboede omr\u00e5der i Uummannaq Fjordsystemet. Der er fortsat stenfaldsaktivitet og sandsynlighed for mindre skredh\u00e6ndelser ved de ustabile fjeldskr\u00e5ninger kortlagt med r\u00f8d farve i figur 1 og 2. Omkring [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":18474,"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":"default","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":43,"footnotes":""},"categories":[2118],"tags":[],"class_list":["post-18477","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\/18477","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\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/comments?post=18477"}],"version-history":[{"count":1,"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/posts\/18477\/revisions"}],"predecessor-version":[{"id":18479,"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/posts\/18477\/revisions\/18479"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/media\/18474"}],"wp:attachment":[{"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/media?parent=18477"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/categories?post=18477"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/govmin.gl\/da\/wp-json\/wp\/v2\/tags?post=18477"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}