{"id":44563,"date":"2026-10-12T11:00:42","date_gmt":"2026-10-12T09:00:42","guid":{"rendered":"https:\/\/resoilfoundation.org\/?p=44563"},"modified":"2026-10-08T13:18:34","modified_gmt":"2026-10-08T11:18:34","slug":"alaska-soil-warming-continuous-permafrost","status":"publish","type":"post","link":"https:\/\/resoilfoundation.org\/en\/environment\/alaska-soil-warming-continuous-permafrost\/","title":{"rendered":"In Alaska, soil is warming faster in regions with continuous permafrost"},"content":{"rendered":"<h2>A study tracks permafrost temperatures from 1997 to 2023, providing new data to forecast thaw and plan infrastructure. Greater depth does not slow the warming trend<\/h2>\n<p style=\"text-align: center;\">by Matteo Cavallito<\/p>\n<p>Alaska\u2019s soil is warming even at depth, with the fastest increases occurring in the Arctic region characterised by continuous <a href=\"https:\/\/resoilfoundation.org\/en\/environment\/near-surface-permafrost-loss-2100\/\" target=\"_blank\" rel=\"noopener\">permafrost<\/a>. These findings come from a <a href=\"https:\/\/www.frontiersin.org\/journals\/climate\/articles\/10.3389\/fclim.2026.1887902\/full\" target=\"_blank\" rel=\"noopener\">study<\/a> by <strong>Washington State University<\/strong>, which analysed temperatures recorded between 1997 and 2023. The findings show that <a href=\"https:\/\/en.wikipedia.org\/wiki\/Polar_amplification\" target=\"_blank\" rel=\"noopener\">polar amplification<\/a>, the phenomenon whereby <strong>warming<\/strong> is more intense at higher latitudes, also extends to soil temperatures.<\/p>\n<p>&#8220;Soil and air temperatures warmed significantly throughout Alaska\u201d, states the study, published in <em>Frontiers in Climate<\/em>. \u201c<strong>Polar amplification<\/strong> was evident in soil temperatures as well as air temperatures, with warming occurring fastest in the continuous permafrost region (the Arctic) and decreasing with latitude&#8221;.<\/p>\n<div class='avia-iframe-wrap'>\n<blockquote class=\"wp-embedded-content\" data-secret=\"skFOyHE0g4\"><p><a href=\"https:\/\/resoilfoundation.org\/en\/articles\/artic-permafrost-microbes-ecosystem\/\">Beneath the Arctic permafrost lies a more complex ecosystem than expected<\/a><\/p><\/blockquote>\n<p><iframe loading=\"lazy\" class=\"wp-embedded-content\" sandbox=\"allow-scripts\" security=\"restricted\" style=\"position: absolute; visibility: hidden;\" title=\"\u201cBeneath the Arctic permafrost lies a more complex ecosystem than expected\u201d \u2014 Re Soil Foundation\" src=\"https:\/\/resoilfoundation.org\/en\/articles\/artic-permafrost-microbes-ecosystem\/embed\/#?secret=XvFFEIMIFf#?secret=skFOyHE0g4\" data-secret=\"skFOyHE0g4\" width=\"600\" height=\"338\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\"><\/iframe><\/div>\n<h5>Understanding how soil responds<\/h5>\n<p>In Alaska, air temperatures <strong>are rising twice as fast<\/strong> as in the contiguous 48 US states. Against this backdrop, understanding how soil responds is essential: <strong>permafrost thaw<\/strong> can lead to the <strong>release of carbon dioxide and methane<\/strong>, fuelling further warming and compromising roads, buildings and pipelines constructed on frozen ground. However, atmospheric warming does not affect soil temperatures to the same extent.<\/p>\n<blockquote><p>&#8220;Although air and soil temperature trends are certainly coupled, they are not interchangeable, because <strong>soils are likely to be buffered<\/strong> from extreme air temperatures during long winters with consistent snow cover&#8221;, the study notes.<\/p><\/blockquote>\n<p>Snow cover insulates the ground, keeping it warmer than the air in winter while also buffering the soil against atmospheric warming. <strong>Moisture, vegetation and landscape features<\/strong> also play a key role. Understanding these processes requires direct measurements, which are difficult to collect across such a vast and often remote territory.<\/p>\n<div class='avia-iframe-wrap'>\n<blockquote class=\"wp-embedded-content\" data-secret=\"c00T2kAE7o\"><p><a href=\"https:\/\/resoilfoundation.org\/en\/articles\/arctic-soil-permafrost-emissions\/\">Here&#8217;s how Arctic soil offsets emissions from alpine permafrost<\/a><\/p><\/blockquote>\n<p><iframe loading=\"lazy\" class=\"wp-embedded-content\" sandbox=\"allow-scripts\" security=\"restricted\" style=\"position: absolute; visibility: hidden;\" title=\"\u201cHere\u2019s how Arctic soil offsets emissions from alpine permafrost\u201d \u2014 Re Soil Foundation\" src=\"https:\/\/resoilfoundation.org\/en\/articles\/arctic-soil-permafrost-emissions\/embed\/#?secret=vExY0sLofl#?secret=c00T2kAE7o\" data-secret=\"c00T2kAE7o\" width=\"600\" height=\"338\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\"><\/iframe><\/div>\n<h5>Soil warms fastest in the continuous permafrost region<\/h5>\n<p>To address this challenge, Washington State researchers Erin E. Oliver and Claire L. Phillips combined <strong>data from 43 weather stations<\/strong>, with records ranging from 10 to 27 years, grouping the stations according to whether they were located in regions with continuous, discontinuous or no permafrost. Soil temperatures were analysed at depths of 5, 20 and 50 centimetres, with measurements at 70, 95 and 120 centimetres included only in the continuous permafrost region. Average soil warming reached <strong>0.64 \u00b0C per decade<\/strong> in the continuous permafrost region, compared with 0.37 \u00b0C in the discontinuous permafrost region and 0.35 \u00b0C in areas without permafrost.<\/p>\n<blockquote><p>In the continuous permafrost region, <strong>air temperatures rose<\/strong> even faster: <strong>1.15 \u00b0C per decade<\/strong>, compared with 0.64 \u00b0C for soil. In the other two regions, the difference between air and soil warming rates was not statistically significant.<\/p><\/blockquote>\n<p>Greater depth, however, <strong>did not slow the warming trend<\/strong>: &#8220;Soil temperatures were warming across the soil profile (measured from 5 to 120 cm in the Arctic, and 5\u201350 cm at lower latitudes) and with no significant differences across measured depths within a region&#8221;, the study reports. &#8220;People tend to think that soil temperatures are more stable as you go deeper. The seasonal fluctuations do drop out, but the long-term warming trend was actually <strong>more obvious at depth<\/strong>&#8220;, <strong>Phillips<\/strong> <a href=\"https:\/\/news.wsu.edu\/press-release\/2026\/10\/01\/in-alaska-soil-in-permafrost-regions-is-warming-the-fastest\/\" target=\"_blank\" rel=\"noopener\">explained<\/a>. In deeper soil layers, temperatures fluctuate less from season to season, making it easier to distinguish long-term warming from normal seasonal variations.<\/p>\n<div class='avia-iframe-wrap'>\n<blockquote class=\"wp-embedded-content\" data-secret=\"VHAni1Gkm6\"><p><a href=\"https:\/\/resoilfoundation.org\/en\/articles\/permafrost-erosion-co2-oceans\/\">Permafrost erosion reduces carbon sequestration in the oceans<\/a><\/p><\/blockquote>\n<p><iframe loading=\"lazy\" class=\"wp-embedded-content\" sandbox=\"allow-scripts\" security=\"restricted\" style=\"position: absolute; visibility: hidden;\" title=\"\u201cPermafrost erosion reduces carbon sequestration in the oceans\u201d \u2014 Re Soil Foundation\" src=\"https:\/\/resoilfoundation.org\/en\/articles\/permafrost-erosion-co2-oceans\/embed\/#?secret=DkEBZLMeDT#?secret=VHAni1Gkm6\" data-secret=\"VHAni1Gkm6\" width=\"600\" height=\"338\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\"><\/iframe><\/div>\n<h5>Snow and seasons help predict changes<\/h5>\n<p>Warming follows <strong>different seasonal patterns<\/strong>. In the continuous permafrost region, the largest increases occur in winter and spring; in the discontinuous permafrost region, mainly in winter; and in areas without permafrost, in summer. <strong>Snow depth<\/strong> also makes a difference: the thicker snowpack in central and southern regions provides greater insulation than the thinner cover in the Arctic region.<\/p>\n<blockquote><p>&#8220;In all three regions, the correlation <strong>was stronger when snow was not present<\/strong> than when it was present. Additionally, snow depth affected the extent of thermal insulation of soil from snow cover&#8221;, the authors write.<\/p><\/blockquote>\n<p>The study thus provides a basis for <strong>improving forecasts<\/strong> of future thaw and informing infrastructure planning. It does not directly measure the emissions but clarifies where and when the ground is warming. Future changes in precipitation and snow cover could alter this response: monitoring air, soil and snow together will therefore be essential to understanding changes in permafrost and guiding adaptation efforts.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>A study tracks permafrost temperatures from 1997 to 2023, providing new data to forecast thaw and plan infrastructure. Greater depth does not slow the warming trend<\/p>\n","protected":false},"author":4,"featured_media":44565,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[144,134],"tags":[301,98,302,318,321,247,188,322,163],"class_list":["post-44563","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-environment","category-articles","tag-carbon-2-en","tag-carbonio","tag-climate-2-en","tag-dissesto-idrogeologico-en","tag-erosione-en","tag-monitoraggio-en","tag-research","tag-suolo-en","tag-usa-en"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v28.5 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>In Alaska, soil is warming faster in continuous permafrost<\/title>\n<meta name=\"description\" content=\"Temperatures are rising even at a depth of 120 centimetres. 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