{"id":3885,"date":"2026-05-19T21:00:17","date_gmt":"2026-05-19T19:00:17","guid":{"rendered":"https:\/\/arcticwatch.info\/index.php\/2026\/05\/19\/facts-about-the-arctic-in-may-2026\/"},"modified":"2026-05-19T21:00:17","modified_gmt":"2026-05-19T19:00:17","slug":"facts-about-the-arctic-in-may-2026","status":"publish","type":"post","link":"https:\/\/arcticwatch.info\/index.php\/2026\/05\/19\/facts-about-the-arctic-in-may-2026\/","title":{"rendered":"Facts About the Arctic in May 2026"},"content":{"rendered":"<div>\n<p>JAXA have updated their visualisations of\u00a0<a href=\"https:\/\/ads.nipr.ac.jp\/vishop\/#\/extent\/\" target=\"_blank\" rel=\"noreferrer noopener\">Arctic sea ice extent<\/a>\u00a0data. The \u201ctraditional\u201d 2 day average graph is now labelled \u201cpreliminary\u201d, and currently shows 2026 in a tie with 2020 for third lowest for the date:<\/p>\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-large\"><a href=\"https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/JAXA-Extent-2026-05-18.png\"><img fetchpriority=\"high\" decoding=\"async\" width=\"1024\" height=\"468\" src=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/JAXA-Extent-2026-05-18-1024x468-1.png\" alt=\"\" class=\"wp-image-37354\" srcset=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/JAXA-Extent-2026-05-18-1024x468-1.png 1024w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/JAXA-Extent-2026-05-18-300x137.png 300w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/JAXA-Extent-2026-05-18-768x351.png 768w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/JAXA-Extent-2026-05-18.png 1111w\" sizes=\"(max-width: 1024px) 100vw, 1024px\"><\/a><\/figure>\n<\/div>\n<p>5 day averaged \u201cconfirmed\u201d data is also available, including regional graphs. By way of example here\u2019s JAXA\u2019s latest extent graph for the Bering Sea, dated May 15th:<\/p>\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-large\"><a href=\"https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/JAXA-Bering-2026-05-15.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"464\" src=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/JAXA-Bering-2026-05-15-1024x464-1.png\" alt=\"\" class=\"wp-image-37355\" srcset=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/JAXA-Bering-2026-05-15-1024x464-1.png 1024w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/JAXA-Bering-2026-05-15-300x136.png 300w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/JAXA-Bering-2026-05-15-768x348.png 768w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/JAXA-Bering-2026-05-15.png 1122w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\"><\/a><\/figure>\n<\/div>\n<p>The Alfred Wegener Institute\u2019s <a href=\"https:\/\/data.seaiceportal.de\/relaunch\/concentration?lang=en\">sea ice concentration data<\/a> reveals open water in the Beaufort, Chukchi, East Siberian and Laptev Seas:<\/p>\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><a href=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/SIC-LEADS_20260518.png\"><img loading=\"lazy\" decoding=\"async\" width=\"850\" height=\"960\" src=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/SIC-LEADS_20260518.png\" alt=\"\" class=\"wp-image-37356\" srcset=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/SIC-LEADS_20260518.png 850w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/SIC-LEADS_20260518-266x300.png 266w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/SIC-LEADS_20260518-768x867.png 768w\" sizes=\"auto, (max-width: 850px) 100vw, 850px\"><\/a><\/figure>\n<\/div>\n<p>In the eastern Beaufort Sea albedo is further reduced by the waters of the Mackenzie River encroaching upon the fast ice off the river delta:<\/p>\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><a href=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/Terra-721-Mackenzie-2026-05-17.jpg\"><img loading=\"lazy\" decoding=\"async\" width=\"868\" height=\"575\" src=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/Terra-721-Mackenzie-2026-05-17.jpg\" alt=\"\" class=\"wp-image-37359\" srcset=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/Terra-721-Mackenzie-2026-05-17.jpg 868w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/Terra-721-Mackenzie-2026-05-17-300x199.jpg 300w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/Terra-721-Mackenzie-2026-05-17-768x509.jpg 768w\" sizes=\"auto, (max-width: 868px) 100vw, 868px\"><\/a><figcaption class=\"wp-element-caption\"><em>\u201cFalse colour\u201d image of the Mackenzie Delta on\u00a0<a href=\"https:\/\/go.nasa.gov\/3RAxdFH\" target=\"_blank\" rel=\"noreferrer noopener\">May 17th<\/a>\u00a0from the MODIS instrument on the Terra satellite<\/em><\/figcaption><\/figure>\n<\/div>\n<p>The monthly summary of atmospheric conditions over the Arctic during April 2026 reveal part of the reason for the open water. A persistent area of high pressure over the Beaufort Sea:<\/p>\n<figure class=\"wp-block-gallery aligncenter has-nested-images columns-default is-cropped wp-block-gallery-1 is-layout-flex wp-block-gallery-is-layout-flex\">\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/ERA5-MSLP-2026-04.jpg\"><img loading=\"lazy\" decoding=\"async\" width=\"688\" height=\"688\" data-id=\"37366\" src=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/ERA5-MSLP-2026-04.jpg\" alt=\"\" class=\"wp-image-37366\" srcset=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/ERA5-MSLP-2026-04.jpg 688w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/ERA5-MSLP-2026-04-300x300.jpg 300w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/ERA5-MSLP-2026-04-150x150.jpg 150w\" sizes=\"auto, (max-width: 688px) 100vw, 688px\"><\/a><\/figure>\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/ERA5-T925-2026-04.jpg\"><img loading=\"lazy\" decoding=\"async\" width=\"688\" height=\"688\" data-id=\"37365\" src=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/ERA5-T925-2026-04.jpg\" alt=\"\" class=\"wp-image-37365\" srcset=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/ERA5-T925-2026-04.jpg 688w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/ERA5-T925-2026-04-300x300.jpg 300w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/ERA5-T925-2026-04-150x150.jpg 150w\" sizes=\"auto, (max-width: 688px) 100vw, 688px\"><\/a><\/figure>\n<\/figure>\n<p>The NSIDC monthly average extent graph for April shows 2026 second lowest behind 2019:<\/p>\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><a href=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/NSIDC-April-2026.png\"><img loading=\"lazy\" decoding=\"async\" width=\"887\" height=\"629\" src=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/NSIDC-April-2026.png\" alt=\"\" class=\"wp-image-37367\" srcset=\"https:\/\/arcticwatch.info\/wp-content\/uploads\/2026\/05\/NSIDC-April-2026.png 887w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/NSIDC-April-2026-300x213.png 300w, https:\/\/greatwhitecon.info\/wp-content\/uploads\/2026\/05\/NSIDC-April-2026-768x545.png 768w\" sizes=\"auto, (max-width: 887px) 100vw, 887px\"><\/a><\/figure>\n<\/div>\n<p>Watch this space!<\/p>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>JAXA have updated their visualisations of\u00a0Arctic sea ice extent\u00a0data. The \u201ctraditional\u201d 2 day average graph is now labelled \u201cpreliminary\u201d, and currently shows 2026 in a tie with 2020 for third lowest for the date: 5 day averaged \u201cconfirmed\u201d data is&#8230;<\/p>\n","protected":false},"author":2,"featured_media":3886,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"rop_custom_images_group":[],"rop_custom_messages_group":[],"rop_publish_now":"initial","rop_publish_now_accounts":[],"rop_publish_now_history":[],"rop_publish_now_status":"pending","_themeisle_gutenberg_block_has_review":false,"footnotes":""},"categories":[1],"tags":[],"class_list":["post-3885","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-uncategorized"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/posts\/3885","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/comments?post=3885"}],"version-history":[{"count":0,"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/posts\/3885\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/media\/3886"}],"wp:attachment":[{"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/media?parent=3885"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/categories?post=3885"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/tags?post=3885"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}