{"id":4277,"date":"2023-09-25T10:51:13","date_gmt":"2023-09-25T08:51:13","guid":{"rendered":"https:\/\/nersc.no\/?p=4277"},"modified":"2023-11-22T09:21:12","modified_gmt":"2023-11-22T08:21:12","slug":"reliable-observations-to-study-sea-level-variations-along-the-coast-of-norway","status":"publish","type":"post","link":"https:\/\/nersc.no\/en\/features\/reliable-observations-to-study-sea-level-variations-along-the-coast-of-norway\/","title":{"rendered":"Reliable observations to study sea-level variations along the coast of Norway"},"content":{"rendered":"<div class=\"wpb-content-wrapper\"><p>[vc_row][vc_column width=&#8221;2\/3&#8243; css=&#8221;.vc_custom_1693479579188{background-color: #ffffff !important;}&#8221;]<div class=\"spacer\" style=\"--space-sm: 25px;--space-md: 25px;--space-lg: 25px;--space-xl: 25px;\"><\/div><div class=\"header left  \"><h1 class=\"heading-2\" title=\"Reliable observations to study sea-level variations along the coast of Norway\">Reliable observations to study sea-level variations along the coast of Norway<\/h1><\/div>[vc_column_text]<strong>Both hydrographic stations and satellites provide reliable observations to study changes in sea level along the Norwegian coast on a month-to-month basis, according to a <\/strong><a href=\"https:\/\/www.nature.com\/articles\/s41598-023-40853-8\" target=\"_blank\" rel=\"noopener\"><strong>new article<\/strong><\/a><strong> by Fabio Mangini and other researchers from the Nansen Center and Sweden. <\/strong><\/p>\n<p>Having reliable information on sea level is especially relevant for coastal communities. Measuring and understanding the variations is therefore an important task. The sea level in a region can change over the course of years, but it also varies over shorter times, such as months.<\/p>\n<p>When measuring the changes in the sea level, researchers distinguish between two components contributing to the total change \u2013 the mass and the steric components. The mass component is altered when the amount of water in a location changes, whereas the steric component is dependent on the density of water, thereby affected by temperature and salinity.<\/p>\n<p>The recent publication by Fabio Mangini and his colleagues focus on the mass component, along the coast of Norway. They set out to investigate if both hydrographic stations and remote sensing instruments can be used to get reliable information on sea-level variations on a month-to-month basis. Along the coastline of Norway, which is thousands of kilometers long, there are only eight such hydrographic stations. They can measure changes in the sea level, but can they provide reliable estimates for such a long coastline? And are satellites circling the globe, doing the same thing but in a different way. Two satellite missions especially, GRACE and GRACE-FO, have caught the interest of Fabio Mangini and his colleagues. These two are generally considered to not be reliable in coastal areas, but they set out to see if this is true.<\/p>\n<p>Fabio Mangini and his colleagues found that even though there are only eight hydrographic stations along the Norwegian coast, the data they measure is reliable to study the <em>overall<\/em> sea-level variations along the coast of Norway. And moreover, they found that the satellite-based information from GRACE and GRACE-FO are just as reliable. Both sources can be used to study the variability of the sea level in the region, and the findings suggest that GRACE and GRACE-FO satellite mission data can also be used to study other coastal areas, not just Norway\u2019s coast. This has important implications for studies of sea-level variations in other parts of the world especially where coastal instruments are absent.<\/p>\n<p>[\/vc_column_text]<div class=\"spacer\" style=\"--space-sm: 30px;--space-md: 30px;--space-lg: 30px;--space-xl: 30px;\"><\/div>[vc_row_inner][vc_column_inner width=&#8221;1\/2&#8243;]\n\t\t\t<figure class=\"standard-image  no-caption left\">\n\t\t\t\t<img loading=\"lazy\" decoding=\"async\" width=\"2048\" height=\"2560\" src=\"https:\/\/nersc.no\/wp-content\/uploads\/2023\/09\/pexels-valdemaras-d-1680381-1-scaled.jpg\" class=\"attachment-img-md size-img-md\" alt=\"\" srcset=\"https:\/\/nersc.no\/wp-content\/uploads\/2023\/09\/pexels-valdemaras-d-1680381-1-scaled.jpg 2048w, https:\/\/nersc.no\/wp-content\/uploads\/2023\/09\/pexels-valdemaras-d-1680381-1-240x300.jpg 240w, https:\/\/nersc.no\/wp-content\/uploads\/2023\/09\/pexels-valdemaras-d-1680381-1-819x1024.jpg 819w, https:\/\/nersc.no\/wp-content\/uploads\/2023\/09\/pexels-valdemaras-d-1680381-1-768x960.jpg 768w, https:\/\/nersc.no\/wp-content\/uploads\/2023\/09\/pexels-valdemaras-d-1680381-1-1229x1536.jpg 1229w, https:\/\/nersc.no\/wp-content\/uploads\/2023\/09\/pexels-valdemaras-d-1680381-1-1638x2048.jpg 1638w, https:\/\/nersc.no\/wp-content\/uploads\/2023\/09\/pexels-valdemaras-d-1680381-1-416x520.jpg 416w, https:\/\/nersc.no\/wp-content\/uploads\/2023\/09\/pexels-valdemaras-d-1680381-1-640x800.jpg 640w, https:\/\/nersc.no\/wp-content\/uploads\/2023\/09\/pexels-valdemaras-d-1680381-1-1280x1600.jpg 1280w, https:\/\/nersc.no\/wp-content\/uploads\/2023\/09\/pexels-valdemaras-d-1680381-1-1536x1920.jpg 1536w\" sizes=\"auto, (max-width: 2048px) 100vw, 2048px\" \/>\n\t\t\t\t\n\t\t\t<\/figure>[\/vc_column_inner][vc_column_inner width=&#8221;1\/2&#8243;][vc_column_text]<\/p>\n<p style=\"text-align: left;\">Photo by Valdemaras D., Pexels<\/p>\n<p>[\/vc_column_text][\/vc_column_inner][\/vc_row_inner][\/vc_column][vc_column width=&#8221;1\/3&#8243; css=&#8221;.vc_custom_1695033709348{padding-right: 0px !important;}&#8221;]<div class=\"spacer\" style=\"--space-sm: 30px;--space-md: 30px;--space-lg: 30px;--space-xl: 30px;\"><\/div><div class=\"infobox teal\">\n<h1>Variasjoner i havniv\u00e5et<\/h1>\n<p>P\u00e5 et bestemt sted varierer havniv\u00e5et over b\u00e5de kort og lang sikt. I korte tidsrom, som for eksempel noen dager, har lufttrykk og vind en effekt p\u00e5 havniv\u00e5et. N\u00e5r man ser p\u00e5 lengre tidsrom, som for eksempel ett \u00e5r, har \u00e5rlige variasjoner i lufttrykket og vannets tetthet som varierer med vanntemperaturen stor p\u00e5virkning p\u00e5 havniv\u00e5et.<\/p><\/div><div class=\"infobox light-blue\">\n<h1>Publikasjon<\/h1>\n<p><strong>Scientific Reports:<\/strong><br \/>\n&#8220;Detection and attribution of intra-annual mass component of sea-level variations along the Norwegian coast&#8221;<\/p><p class=\"textlink left\"><a href=\"https:\/\/doi.org\/10.1038\/s41598-023-40853-8\" title=\"Les artikkelen\" target=\"_blank\" rel=\"noopener\">Les artikkelen<img decoding=\"async\" src=\"\/wp-content\/themes\/ppcore\/assets\/images\/white-arrow.svg\" alt=\"Pil icon\" aria-hidden=\"true\"><\/a><\/p><\/div>[\/vc_column][\/vc_row]<\/p>\n<\/div>","protected":false},"excerpt":{"rendered":"<p>[vc_row][vc_column width=&#8221;2\/3&#8243; css=&#8221;.vc_custom_1693479579188{background-color: #ffffff !important;}&#8221;][vc_column_text]Both hydrographic stations and satellites provide reliable observations to study changes in sea level along the Norwegian coast on a month-to-month basis, according to a new article by Fabio Mangini and other researchers from the Nansen Center and Sweden. Having reliable information on sea level is especially relevant for coastal communities. [&hellip;]<\/p>\n","protected":false},"author":4,"featured_media":2293,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"_relevanssi_hide_post":"","_relevanssi_hide_content":"","_relevanssi_pin_for_all":"","_relevanssi_pin_keywords":"","_relevanssi_unpin_keywords":"","_relevanssi_related_keywords":"","_relevanssi_related_include_ids":"","_relevanssi_related_exclude_ids":"","_relevanssi_related_no_append":"","_relevanssi_related_not_related":"","_relevanssi_related_posts":"","_relevanssi_noindex_reason":"","footnotes":""},"categories":[80],"tags":[],"class_list":["post-4277","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-features"],"acf":[],"publishpress_future_action":{"enabled":false,"date":"2026-05-08 11:56:51","action":"change-status","newStatus":"draft","terms":[],"taxonomy":"category","extraData":[]},"publishpress_future_workflow_manual_trigger":{"enabledWorkflows":[]},"_links":{"self":[{"href":"https:\/\/nersc.no\/en\/wp-json\/wp\/v2\/posts\/4277","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/nersc.no\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/nersc.no\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/nersc.no\/en\/wp-json\/wp\/v2\/users\/4"}],"replies":[{"embeddable":true,"href":"https:\/\/nersc.no\/en\/wp-json\/wp\/v2\/comments?post=4277"}],"version-history":[{"count":2,"href":"https:\/\/nersc.no\/en\/wp-json\/wp\/v2\/posts\/4277\/revisions"}],"predecessor-version":[{"id":5958,"href":"https:\/\/nersc.no\/en\/wp-json\/wp\/v2\/posts\/4277\/revisions\/5958"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/nersc.no\/en\/wp-json\/wp\/v2\/media\/2293"}],"wp:attachment":[{"href":"https:\/\/nersc.no\/en\/wp-json\/wp\/v2\/media?parent=4277"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/nersc.no\/en\/wp-json\/wp\/v2\/categories?post=4277"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/nersc.no\/en\/wp-json\/wp\/v2\/tags?post=4277"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}