{"id":1826,"date":"2016-09-01T14:52:25","date_gmt":"1970-01-01T00:00:00","guid":{"rendered":"https:\/\/nis.gl\/projekt\/extreme-weather-in-west-greenland-frequency-magnitude-and-impact\/"},"modified":"2016-09-01T14:52:25","modified_gmt":"1970-01-01T00:00:00","slug":"extreme-weather-in-west-greenland-frequency-magnitude-and-impact","status":"publish","type":"projekt","link":"https:\/\/nis.gl\/en\/projekt\/extreme-weather-in-west-greenland-frequency-magnitude-and-impact\/","title":{"rendered":"Extreme Weather in West Greenland \u2013 Frequency, Magnitude and Impact"},"content":{"rendered":"<p><strong>Projektleder:<br \/>\n<\/strong>Jakob Abermann<\/p>\n<p><strong>Fakultet \/ Forskningsinstitution:<br \/>\n<\/strong>Naturvidenskab \/ Asiaq<\/p>\n<p><strong>Titel:<br \/>\n<\/strong>Extreme Weather in West Greenland \u2013 Frequency, Magnitude and Impact<\/p>\n<p><strong>Beskrivelse:<br \/>\n<\/strong>Heavy precipitation (ca. 30 mm) along with an impressive temperature rise (almost 26\u00b0C in 60 hours) and abnormally warm temperatures (up to 18.1\u00b0C) occurred between 9 April and 11 April 2016 in Kangerluarsunnguaq. Within 24 hours, the water level, since the temperature rise and likely an unstable snow pack, we observed a number of avalanches that in parts also destroyed some of our monitoring installations. Reviewing the literature, we found that the type of avalanches is best characterized as a \u2018slush flow\u2019, defined as a \u2018mudflow-like flowage of water-saturated snow\u2019. Perquisites are heavy precipitation and high temperatures. Such extreme events are a hazard for infrastructure, and a along with the recent warming in Greenland, there are indications that their frequency increases which makes their understating vital for adaptation measures.<\/p>\n<p>The aim of this project is therefore to:<\/p>\n<ol>\n<li>quantify an extreme event in West Greenland, and describe conditions that lead to that,<\/li>\n<li>assess the potential of Remote Sensing methods for defining the spatial extent of the April 2016 event.<\/li>\n<\/ol>\n<p>Once (I) and (II) have been answered, our longer climate time series will allow for assessment of recurrence times.<\/p>\n<p><strong>Rapport og opg\u00f8relse:<br \/>\n<\/strong><a href=\"https:\/\/nis.gl\/wp-content\/uploads\/2020\/08\/Final-Report_ExtremeEv_Abermann.pdf\" target=\"_blank\" rel=\"noopener noreferrer\">Extreme Weather in West Greenland \u2013 Frequency, Magnitude, and Impact<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Projektleder: Jakob Abermann Fakultet \/ Forskningsinstitution: Naturvidenskab \/ Asiaq Titel: Extreme Weather in West Greenland \u2013 Frequency, Magnitude and Impact Beskrivelse: Heavy precipitation (ca. 30 mm) along with an impressive temperature rise (almost 26\u00b0C in 60 hours) and abnormally warm temperatures (up to 18.1\u00b0C) occurred between 9 April and 11 April 2016 in Kangerluarsunnguaq. Within [&hellip;]<\/p>\n","protected":false},"parent":0,"menu_order":0,"template":"","meta":{"_acf_changed":false,"site-sidebar-layout":"default","site-content-layout":"default","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":"","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":""}}},"_years":[182],"kategori":[171],"pulje":[160],"projektleder":[],"fakultet":[147],"institution":[],"class_list":["post-1826","projekt","type-projekt","status-publish","hentry","_years-2016-en","kategori-research-promotion","pulje-pool-2","fakultet-science"],"acf":[],"ptb_metabox":[],"ptb_taxonomy":{"_years":[{"term_id":182,"name":"2016","slug":"2016-en","term_group":4,"term_taxonomy_id":182,"taxonomy":"_years","description":"","parent":0,"count":16,"filter":"raw"}],"kategori":[{"term_id":171,"name":"Research Promotion","slug":"research-promotion","term_group":4,"term_taxonomy_id":171,"taxonomy":"kategori","description":"","parent":0,"count":101,"filter":"raw"}],"pulje":[{"term_id":160,"name":"Pool 2","slug":"pool-2","term_group":4,"term_taxonomy_id":160,"taxonomy":"pulje","description":"","parent":0,"count":36,"filter":"raw"}],"fakultet":[{"term_id":147,"name":"Natural Sciences","slug":"science","term_group":4,"term_taxonomy_id":147,"taxonomy":"fakultet","description":"","parent":0,"count":83,"filter":"raw"}]},"ptb_featured_image":null,"_links":{"self":[{"href":"https:\/\/nis.gl\/en\/wp-json\/wp\/v2\/projekt\/1826","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/nis.gl\/en\/wp-json\/wp\/v2\/projekt"}],"about":[{"href":"https:\/\/nis.gl\/en\/wp-json\/wp\/v2\/types\/projekt"}],"wp:attachment":[{"href":"https:\/\/nis.gl\/en\/wp-json\/wp\/v2\/media?parent=1826"}],"wp:term":[{"taxonomy":"_years","embeddable":true,"href":"https:\/\/nis.gl\/en\/wp-json\/wp\/v2\/_years?post=1826"},{"taxonomy":"kategori","embeddable":true,"href":"https:\/\/nis.gl\/en\/wp-json\/wp\/v2\/kategori?post=1826"},{"taxonomy":"pulje","embeddable":true,"href":"https:\/\/nis.gl\/en\/wp-json\/wp\/v2\/pulje?post=1826"},{"taxonomy":"projektleder","embeddable":true,"href":"https:\/\/nis.gl\/en\/wp-json\/wp\/v2\/projektleder?post=1826"},{"taxonomy":"fakultet","embeddable":true,"href":"https:\/\/nis.gl\/en\/wp-json\/wp\/v2\/fakultet?post=1826"},{"taxonomy":"institution","embeddable":true,"href":"https:\/\/nis.gl\/en\/wp-json\/wp\/v2\/institution?post=1826"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}