{"id":415643,"date":"2025-12-02T08:39:51","date_gmt":"2025-12-02T07:39:51","guid":{"rendered":"https:\/\/climatescience.press\/?p=415643"},"modified":"2025-12-26T02:44:26","modified_gmt":"2025-12-26T01:44:26","slug":"two-hot-spots-slow-arctic-ice-recovery-november-2025","status":"publish","type":"post","link":"https:\/\/climatescience.press\/?p=415643","title":{"rendered":"Two Hot Spots Slow Arctic Ice Recovery November\u00a02025"},"content":{"rendered":"\n<figure class=\"wp-block-image size-large\"><img data-recalc-dims=\"1\" loading=\"lazy\" decoding=\"async\" width=\"723\" height=\"406\" data-attachment-id=\"415657\" data-permalink=\"https:\/\/climatescience.press\/?attachment_id=415657\" data-orig-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/0AQNMJtXDkR1sOsNE_BvU44yKuoBaYELvJFcMjgGCXdd5Nh58zuo7omKxhAXfoXGoWw7XcY8gK6QwBTIq5UtwwUdfSSHBFo2Sj4EC_Geuk-zf9cW2RKdATC4dBCZLIL8-1.jpeg?fit=1543%2C866&amp;ssl=1\" data-orig-size=\"1543,866\" data-comments-opened=\"1\" data-image-meta=\"{&quot;aperture&quot;:&quot;0&quot;,&quot;credit&quot;:&quot;&quot;,&quot;camera&quot;:&quot;&quot;,&quot;caption&quot;:&quot;&quot;,&quot;created_timestamp&quot;:&quot;0&quot;,&quot;copyright&quot;:&quot;&quot;,&quot;focal_length&quot;:&quot;0&quot;,&quot;iso&quot;:&quot;0&quot;,&quot;shutter_speed&quot;:&quot;0&quot;,&quot;title&quot;:&quot;&quot;,&quot;orientation&quot;:&quot;0&quot;}\" data-image-title=\"0,AQNMJtXDkR1sOsNE_BvU44yKuoBaYELvJFcMjgGCXdd5Nh58zuo7omKxhAXfoXGoWw7XcY8gK6QwBTIq5UtwwUdfSSHBFo2Sj4EC_Geuk-zf9cW2RKdATC4dBCZLIL8 (1)\" data-image-description=\"\" data-image-caption=\"\" data-large-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/0AQNMJtXDkR1sOsNE_BvU44yKuoBaYELvJFcMjgGCXdd5Nh58zuo7omKxhAXfoXGoWw7XcY8gK6QwBTIq5UtwwUdfSSHBFo2Sj4EC_Geuk-zf9cW2RKdATC4dBCZLIL8-1.jpeg?fit=723%2C406&amp;ssl=1\" src=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/0AQNMJtXDkR1sOsNE_BvU44yKuoBaYELvJFcMjgGCXdd5Nh58zuo7omKxhAXfoXGoWw7XcY8gK6QwBTIq5UtwwUdfSSHBFo2Sj4EC_Geuk-zf9cW2RKdATC4dBCZLIL8-1.jpeg?resize=723%2C406&#038;ssl=1\" alt=\"A research vessel navigating through a vast expanse of Arctic sea ice under clear blue skies.\" class=\"wp-image-415657\" srcset=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/0AQNMJtXDkR1sOsNE_BvU44yKuoBaYELvJFcMjgGCXdd5Nh58zuo7omKxhAXfoXGoWw7XcY8gK6QwBTIq5UtwwUdfSSHBFo2Sj4EC_Geuk-zf9cW2RKdATC4dBCZLIL8-1.jpeg?resize=1024%2C575&amp;ssl=1 1024w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/0AQNMJtXDkR1sOsNE_BvU44yKuoBaYELvJFcMjgGCXdd5Nh58zuo7omKxhAXfoXGoWw7XcY8gK6QwBTIq5UtwwUdfSSHBFo2Sj4EC_Geuk-zf9cW2RKdATC4dBCZLIL8-1.jpeg?resize=300%2C168&amp;ssl=1 300w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/0AQNMJtXDkR1sOsNE_BvU44yKuoBaYELvJFcMjgGCXdd5Nh58zuo7omKxhAXfoXGoWw7XcY8gK6QwBTIq5UtwwUdfSSHBFo2Sj4EC_Geuk-zf9cW2RKdATC4dBCZLIL8-1.jpeg?resize=768%2C431&amp;ssl=1 768w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/0AQNMJtXDkR1sOsNE_BvU44yKuoBaYELvJFcMjgGCXdd5Nh58zuo7omKxhAXfoXGoWw7XcY8gK6QwBTIq5UtwwUdfSSHBFo2Sj4EC_Geuk-zf9cW2RKdATC4dBCZLIL8-1.jpeg?resize=1536%2C862&amp;ssl=1 1536w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/0AQNMJtXDkR1sOsNE_BvU44yKuoBaYELvJFcMjgGCXdd5Nh58zuo7omKxhAXfoXGoWw7XcY8gK6QwBTIq5UtwwUdfSSHBFo2Sj4EC_Geuk-zf9cW2RKdATC4dBCZLIL8-1.jpeg?resize=640%2C359&amp;ssl=1 640w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/0AQNMJtXDkR1sOsNE_BvU44yKuoBaYELvJFcMjgGCXdd5Nh58zuo7omKxhAXfoXGoWw7XcY8gK6QwBTIq5UtwwUdfSSHBFo2Sj4EC_Geuk-zf9cW2RKdATC4dBCZLIL8-1.jpeg?resize=1200%2C673&amp;ssl=1 1200w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/0AQNMJtXDkR1sOsNE_BvU44yKuoBaYELvJFcMjgGCXdd5Nh58zuo7omKxhAXfoXGoWw7XcY8gK6QwBTIq5UtwwUdfSSHBFo2Sj4EC_Geuk-zf9cW2RKdATC4dBCZLIL8-1.jpeg?w=1543&amp;ssl=1 1543w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/0AQNMJtXDkR1sOsNE_BvU44yKuoBaYELvJFcMjgGCXdd5Nh58zuo7omKxhAXfoXGoWw7XcY8gK6QwBTIq5UtwwUdfSSHBFo2Sj4EC_Geuk-zf9cW2RKdATC4dBCZLIL8-1.jpeg?w=1446&amp;ssl=1 1446w\" sizes=\"auto, (max-width: 723px) 100vw, 723px\" \/><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">From <a href=\"https:\/\/rclutz.com\/2025\/12\/01\/two-hot-spots-slow-arctic-ice-recovery-november-2025\/\">Science Matters<\/a><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">By\u00a0<a href=\"https:\/\/rclutz.com\/author\/ronaldrc\/\">Ron Clutz<\/a><\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img data-recalc-dims=\"1\" loading=\"lazy\" decoding=\"async\" width=\"723\" height=\"333\" data-attachment-id=\"415645\" data-permalink=\"https:\/\/climatescience.press\/?attachment_id=415645\" data-orig-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-27.png?fit=1430%2C658&amp;ssl=1\" data-orig-size=\"1430,658\" data-comments-opened=\"1\" data-image-meta=\"{&quot;aperture&quot;:&quot;0&quot;,&quot;credit&quot;:&quot;&quot;,&quot;camera&quot;:&quot;&quot;,&quot;caption&quot;:&quot;&quot;,&quot;created_timestamp&quot;:&quot;0&quot;,&quot;copyright&quot;:&quot;&quot;,&quot;focal_length&quot;:&quot;0&quot;,&quot;iso&quot;:&quot;0&quot;,&quot;shutter_speed&quot;:&quot;0&quot;,&quot;title&quot;:&quot;&quot;,&quot;orientation&quot;:&quot;0&quot;}\" data-image-title=\"image\" data-image-description=\"\" data-image-caption=\"\" data-large-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-27.png?fit=723%2C333&amp;ssl=1\" src=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-27.png?resize=723%2C333&#038;ssl=1\" alt=\"Two weather forecast maps showing GPH and temperature anomalies for the Northern Hemisphere. The left map illustrates the 1-5 day forecast, while the right shows the 11-15 day forecast.\" class=\"wp-image-415645\" srcset=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-27.png?resize=1024%2C471&amp;ssl=1 1024w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-27.png?resize=300%2C138&amp;ssl=1 300w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-27.png?resize=768%2C353&amp;ssl=1 768w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-27.png?resize=640%2C294&amp;ssl=1 640w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-27.png?resize=1200%2C552&amp;ssl=1 1200w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-27.png?w=1430&amp;ssl=1 1430w\" sizes=\"auto, (max-width: 723px) 100vw, 723px\" \/><figcaption class=\"wp-element-caption\">Figure 12. (a) Predicted 10 mb geopotential heights (dam; contours) and temperature anomalies (\u00b0C; shading) across the Northern Hemisphere averaged for 25 Nov to 29 Nov 2025. (b) Same as (a) except forecasted averaged from 05 Dec to 09 Dec 2025. The forecasts are from the 00Z 24 November 2025 GFS model ensemble.<\/figcaption><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">The polar vortex is pronounced this year, resulting in warmer temperature over the Arctic ocean, and slowing the normal sea ice recovery.&nbsp; Dr. Judah Cohen at&nbsp;<a href=\"https:\/\/published.aer.com\/aoblog\/aoblog.html\"><strong>AER Arctic Oscillation<\/strong><\/a>&nbsp;blog provides information like the chart above.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">After a pattern of solidly growing sea ice extent in October, a slowdown occurred in November, coincidental with the warm spots shown above.&nbsp; The graph below shows 2025 compared to the 19 year average (2006 to 2024 inclusive), to SII (Sea Ice Index) and some notable years.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img data-recalc-dims=\"1\" loading=\"lazy\" decoding=\"async\" width=\"723\" height=\"473\" data-attachment-id=\"415647\" data-permalink=\"https:\/\/climatescience.press\/?attachment_id=415647\" data-orig-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-28.png?fit=1008%2C659&amp;ssl=1\" data-orig-size=\"1008,659\" data-comments-opened=\"1\" data-image-meta=\"{&quot;aperture&quot;:&quot;0&quot;,&quot;credit&quot;:&quot;&quot;,&quot;camera&quot;:&quot;&quot;,&quot;caption&quot;:&quot;&quot;,&quot;created_timestamp&quot;:&quot;0&quot;,&quot;copyright&quot;:&quot;&quot;,&quot;focal_length&quot;:&quot;0&quot;,&quot;iso&quot;:&quot;0&quot;,&quot;shutter_speed&quot;:&quot;0&quot;,&quot;title&quot;:&quot;&quot;,&quot;orientation&quot;:&quot;0&quot;}\" data-image-title=\"image\" data-image-description=\"\" data-image-caption=\"\" data-large-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-28.png?fit=723%2C473&amp;ssl=1\" src=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-28.png?resize=723%2C473&#038;ssl=1\" alt=\"Line graph displaying November Arctic ice extents in million square kilometers, comparing 2025, 2024, 2020, 2007, and 19-year averages.\" class=\"wp-image-415647\" srcset=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-28.png?w=1008&amp;ssl=1 1008w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-28.png?resize=300%2C196&amp;ssl=1 300w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-28.png?resize=768%2C502&amp;ssl=1 768w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-28.png?resize=640%2C418&amp;ssl=1 640w\" sizes=\"auto, (max-width: 723px) 100vw, 723px\" \/><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">According to MASIE. the average November adds ~2.5M km2 of sea ice extent, which is matched also by 2007.\u00a0 2024 started below average, but gained steadily to close the gap.\u00a0 2025 started at the same level, but the refreezing slowed down, ending November in deficit by 1.1M km2.\u00a0 SII shows even lower ice extents (the last two days not yet reported.)<\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><img data-recalc-dims=\"1\" loading=\"lazy\" decoding=\"async\" width=\"625\" height=\"430\" data-attachment-id=\"415649\" data-permalink=\"https:\/\/climatescience.press\/?attachment_id=415649\" data-orig-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-30.png?fit=625%2C430&amp;ssl=1\" data-orig-size=\"625,430\" data-comments-opened=\"1\" data-image-meta=\"{&quot;aperture&quot;:&quot;0&quot;,&quot;credit&quot;:&quot;&quot;,&quot;camera&quot;:&quot;&quot;,&quot;caption&quot;:&quot;&quot;,&quot;created_timestamp&quot;:&quot;0&quot;,&quot;copyright&quot;:&quot;&quot;,&quot;focal_length&quot;:&quot;0&quot;,&quot;iso&quot;:&quot;0&quot;,&quot;shutter_speed&quot;:&quot;0&quot;,&quot;title&quot;:&quot;&quot;,&quot;orientation&quot;:&quot;0&quot;}\" data-image-title=\"image\" data-image-description=\"\" data-image-caption=\"\" data-large-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-30.png?fit=625%2C430&amp;ssl=1\" src=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-30.png?resize=625%2C430&#038;ssl=1\" alt=\"A cartoon depicting a polar bear next to an out-of-order ice maker, expressing concern about ice levels while a person in winter attire holds a sign stating 'The Earth has a fever.'\" class=\"wp-image-415649\" srcset=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-30.png?w=625&amp;ssl=1 625w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-30.png?resize=300%2C206&amp;ssl=1 300w\" sizes=\"auto, (max-width: 625px) 100vw, 625px\" \/><\/figure>\n<\/div>\n\n\n<p class=\"wp-block-paragraph\">The table below shows the distribution of ice in the Arctic Ocean basins, suggesting two places where ice recovery is lagging.<\/p>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"has-fixed-layout\"><tbody><tr><td class=\"has-text-align-center\" data-align=\"center\"><strong>Region<\/strong><\/td><td class=\"has-text-align-center\" data-align=\"center\"><strong>2025334<\/strong><\/td><td class=\"has-text-align-center\" data-align=\"center\"><strong>Day 334 Ave.<\/strong><\/td><td class=\"has-text-align-center\" data-align=\"center\"><strong>2025-Ave.<\/strong><\/td><td class=\"has-text-align-center\" data-align=\"center\"><strong>2007334<\/strong><\/td><td class=\"has-text-align-center\" data-align=\"center\"><strong>2025-2007<\/strong><\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(0) Northern_Hemisphere<\/td><td class=\"has-text-align-right\" data-align=\"right\">9784037<\/td><td class=\"has-text-align-right\" data-align=\"right\">10880420<\/td><td class=\"has-text-align-right\" data-align=\"right\">-1096383<\/td><td class=\"has-text-align-right\" data-align=\"right\">11009948<\/td><td class=\"has-text-align-right\" data-align=\"right\">-1225911<\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(1) Beaufort_Sea<\/td><td class=\"has-text-align-right\" data-align=\"right\">1071070<\/td><td class=\"has-text-align-right\" data-align=\"right\">1069623<\/td><td class=\"has-text-align-right\" data-align=\"right\">1447<\/td><td class=\"has-text-align-right\" data-align=\"right\">1058872<\/td><td class=\"has-text-align-right\" data-align=\"right\">12198<\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(2) Chukchi_Sea<\/td><td class=\"has-text-align-right\" data-align=\"right\">879082<\/td><td class=\"has-text-align-right\" data-align=\"right\">791207<\/td><td class=\"has-text-align-right\" data-align=\"right\">87875<\/td><td class=\"has-text-align-right\" data-align=\"right\">687829<\/td><td class=\"has-text-align-right\" data-align=\"right\">191253<\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(3) East_Siberian_Sea<\/td><td class=\"has-text-align-right\" data-align=\"right\">1087137<\/td><td class=\"has-text-align-right\" data-align=\"right\">1083943<\/td><td class=\"has-text-align-right\" data-align=\"right\">3194<\/td><td class=\"has-text-align-right\" data-align=\"right\">1082015<\/td><td class=\"has-text-align-right\" data-align=\"right\">5122<\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(4) Laptev_Sea<\/td><td class=\"has-text-align-right\" data-align=\"right\">897845<\/td><td class=\"has-text-align-right\" data-align=\"right\">897824<\/td><td class=\"has-text-align-right\" data-align=\"right\">21<\/td><td class=\"has-text-align-right\" data-align=\"right\">897613<\/td><td class=\"has-text-align-right\" data-align=\"right\">232<\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(5) Kara_Sea<\/td><td class=\"has-text-align-right\" data-align=\"right\">565299<\/td><td class=\"has-text-align-right\" data-align=\"right\">792107<\/td><td class=\"has-text-align-right\" data-align=\"right\">-226808<\/td><td class=\"has-text-align-right\" data-align=\"right\">826319<\/td><td class=\"has-text-align-right\" data-align=\"right\">-261020<\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(6) Barents_Sea<\/td><td class=\"has-text-align-right\" data-align=\"right\">28050<\/td><td class=\"has-text-align-right\" data-align=\"right\">242740<\/td><td class=\"has-text-align-right\" data-align=\"right\">-214690<\/td><td class=\"has-text-align-right\" data-align=\"right\">216525<\/td><td class=\"has-text-align-right\" data-align=\"right\">-188474<\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(7) Greenland_Sea<\/td><td class=\"has-text-align-right\" data-align=\"right\">550413<\/td><td class=\"has-text-align-right\" data-align=\"right\">539687<\/td><td class=\"has-text-align-right\" data-align=\"right\">10726<\/td><td class=\"has-text-align-right\" data-align=\"right\">618844<\/td><td class=\"has-text-align-right\" data-align=\"right\">-68431<\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(8) Baffin_Bay_Gulf_of_St._Lawrence<\/td><td class=\"has-text-align-right\" data-align=\"right\">412284<\/td><td class=\"has-text-align-right\" data-align=\"right\">664437<\/td><td class=\"has-text-align-right\" data-align=\"right\">-252153<\/td><td class=\"has-text-align-right\" data-align=\"right\">708497<\/td><td class=\"has-text-align-right\" data-align=\"right\">-296212<\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(9) Canadian_Archipelago<\/td><td class=\"has-text-align-right\" data-align=\"right\">854931<\/td><td class=\"has-text-align-right\" data-align=\"right\">853431<\/td><td class=\"has-text-align-right\" data-align=\"right\">1500<\/td><td class=\"has-text-align-right\" data-align=\"right\">850249<\/td><td class=\"has-text-align-right\" data-align=\"right\">4682<\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(10) Hudson_Bay<\/td><td class=\"has-text-align-right\" data-align=\"right\">188797<\/td><td class=\"has-text-align-right\" data-align=\"right\">543322<\/td><td class=\"has-text-align-right\" data-align=\"right\">-354525<\/td><td class=\"has-text-align-right\" data-align=\"right\">751382<\/td><td class=\"has-text-align-right\" data-align=\"right\">-562585<\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(11) Central_Arctic<\/td><td class=\"has-text-align-right\" data-align=\"right\">3037637<\/td><td class=\"has-text-align-right\" data-align=\"right\">3193296<\/td><td class=\"has-text-align-right\" data-align=\"right\">-155659<\/td><td class=\"has-text-align-right\" data-align=\"right\">3183072.72<\/td><td class=\"has-text-align-right\" data-align=\"right\">-145436<\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(12) Bering_Sea<\/td><td class=\"has-text-align-right\" data-align=\"right\">145331<\/td><td class=\"has-text-align-right\" data-align=\"right\">138776<\/td><td class=\"has-text-align-right\" data-align=\"right\">6555<\/td><td class=\"has-text-align-right\" data-align=\"right\">72644.62<\/td><td class=\"has-text-align-right\" data-align=\"right\">72687<\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(13) Baltic_Sea<\/td><td class=\"has-text-align-right\" data-align=\"right\">4226<\/td><td class=\"has-text-align-right\" data-align=\"right\">4452<\/td><td class=\"has-text-align-right\" data-align=\"right\">-225<\/td><td class=\"has-text-align-right\" data-align=\"right\">0<\/td><td class=\"has-text-align-right\" data-align=\"right\">4226<\/td><\/tr><tr><td class=\"has-text-align-left\" data-align=\"left\">&nbsp;(14) Sea_of_Okhotsk<\/td><td class=\"has-text-align-right\" data-align=\"right\">58288<\/td><td class=\"has-text-align-right\" data-align=\"right\">61277<\/td><td class=\"has-text-align-right\" data-align=\"right\">-2989<\/td><td class=\"has-text-align-right\" data-align=\"right\">53052<\/td><td class=\"has-text-align-right\" data-align=\"right\">5236<\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">Overall ice extent was 1.1M km2 below average or 10%.&nbsp; About half the deficit comes from the European Atlantic basins, Kara and Barents seas.&nbsp; The other half is mostly from N. America\u2019s Hudson and Baffin bays. Ice in these regions operate on the LIFO principle, last in and first out.<\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><img data-recalc-dims=\"1\" loading=\"lazy\" decoding=\"async\" width=\"562\" height=\"584\" data-attachment-id=\"415652\" data-permalink=\"https:\/\/climatescience.press\/?attachment_id=415652\" data-orig-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-32.png?fit=562%2C584&amp;ssl=1\" data-orig-size=\"562,584\" data-comments-opened=\"1\" data-image-meta=\"{&quot;aperture&quot;:&quot;0&quot;,&quot;credit&quot;:&quot;&quot;,&quot;camera&quot;:&quot;&quot;,&quot;caption&quot;:&quot;&quot;,&quot;created_timestamp&quot;:&quot;0&quot;,&quot;copyright&quot;:&quot;&quot;,&quot;focal_length&quot;:&quot;0&quot;,&quot;iso&quot;:&quot;0&quot;,&quot;shutter_speed&quot;:&quot;0&quot;,&quot;title&quot;:&quot;&quot;,&quot;orientation&quot;:&quot;0&quot;}\" data-image-title=\"image\" data-image-description=\"\" data-image-caption=\"\" data-large-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-32.png?fit=562%2C584&amp;ssl=1\" src=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-32.png?resize=562%2C584&#038;ssl=1\" alt=\"Map of the Arctic region showing various seas and countries including the United States, Canada, Greenland, and Russia.\" class=\"wp-image-415652\" srcset=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-32.png?w=562&amp;ssl=1 562w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-32.png?resize=289%2C300&amp;ssl=1 289w\" sizes=\"auto, (max-width: 562px) 100vw, 562px\" \/><\/figure>\n<\/div>\n\n\n<p class=\"wp-block-paragraph\">At this point in the year, Arctic ice has grown back to 65% of last March maximum with 2.5 months to catch up.\u00a0 \u00a0AER\u00a0 suggests that things may shift again in December:<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img data-recalc-dims=\"1\" loading=\"lazy\" decoding=\"async\" width=\"723\" height=\"237\" data-attachment-id=\"415653\" data-permalink=\"https:\/\/climatescience.press\/?attachment_id=415653\" data-orig-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-33.png?fit=4356%2C1427&amp;ssl=1\" data-orig-size=\"4356,1427\" data-comments-opened=\"1\" data-image-meta=\"{&quot;aperture&quot;:&quot;0&quot;,&quot;credit&quot;:&quot;&quot;,&quot;camera&quot;:&quot;&quot;,&quot;caption&quot;:&quot;&quot;,&quot;created_timestamp&quot;:&quot;0&quot;,&quot;copyright&quot;:&quot;&quot;,&quot;focal_length&quot;:&quot;0&quot;,&quot;iso&quot;:&quot;0&quot;,&quot;shutter_speed&quot;:&quot;0&quot;,&quot;title&quot;:&quot;&quot;,&quot;orientation&quot;:&quot;0&quot;}\" data-image-title=\"image\" data-image-description=\"\" data-image-caption=\"\" data-large-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-33.png?fit=723%2C237&amp;ssl=1\" src=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-33.png?resize=723%2C237&#038;ssl=1\" alt=\"Map showing temperature anomalies from November 24 to December 9, 2025, with warmer temperatures indicated in red and cooler temperatures in blue across North America and parts of Europe and Asia.\" class=\"wp-image-415653\" srcset=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-33.png?resize=1024%2C335&amp;ssl=1 1024w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-33.png?resize=300%2C98&amp;ssl=1 300w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-33.png?resize=768%2C252&amp;ssl=1 768w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-33.png?resize=1536%2C503&amp;ssl=1 1536w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-33.png?resize=2048%2C671&amp;ssl=1 2048w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-33.png?resize=640%2C210&amp;ssl=1 640w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-33.png?resize=1200%2C393&amp;ssl=1 1200w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-33.png?w=1446&amp;ssl=1 1446w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-33.png?w=2169&amp;ssl=1 2169w\" sizes=\"auto, (max-width: 723px) 100vw, 723px\" \/><figcaption class=\"wp-element-caption\">Figure 9. Forecasted surface temperature anomalies (\u00b0C; shading) from 05 Dec to 09 Dec 2025. The forecasts are from the 00Z 24 Nov 2025 GFS ensemble.<\/figcaption><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img data-recalc-dims=\"1\" loading=\"lazy\" decoding=\"async\" width=\"723\" height=\"229\" data-attachment-id=\"415654\" data-permalink=\"https:\/\/climatescience.press\/?attachment_id=415654\" data-orig-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-34.png?fit=3492%2C1104&amp;ssl=1\" data-orig-size=\"3492,1104\" data-comments-opened=\"1\" data-image-meta=\"{&quot;aperture&quot;:&quot;0&quot;,&quot;credit&quot;:&quot;&quot;,&quot;camera&quot;:&quot;&quot;,&quot;caption&quot;:&quot;&quot;,&quot;created_timestamp&quot;:&quot;0&quot;,&quot;copyright&quot;:&quot;&quot;,&quot;focal_length&quot;:&quot;0&quot;,&quot;iso&quot;:&quot;0&quot;,&quot;shutter_speed&quot;:&quot;0&quot;,&quot;title&quot;:&quot;&quot;,&quot;orientation&quot;:&quot;0&quot;}\" data-image-title=\"image\" data-image-description=\"\" data-image-caption=\"\" data-large-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-34.png?fit=723%2C229&amp;ssl=1\" src=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-34.png?resize=723%2C229&#038;ssl=1\" alt=\"Map showing the GEFS 11-15 Day Forecast of Snow Water Equivalent (SNOD) change from November 24 to December 9, 2025, with regions highlighted in blue indicating snowfall increase and red indicating decrease.\" class=\"wp-image-415654\" srcset=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-34.png?resize=1024%2C324&amp;ssl=1 1024w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-34.png?resize=300%2C95&amp;ssl=1 300w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-34.png?resize=768%2C243&amp;ssl=1 768w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-34.png?resize=1536%2C486&amp;ssl=1 1536w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-34.png?resize=2048%2C647&amp;ssl=1 2048w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-34.png?resize=640%2C202&amp;ssl=1 640w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-34.png?resize=1200%2C379&amp;ssl=1 1200w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-34.png?w=1446&amp;ssl=1 1446w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/image-34.png?w=2169&amp;ssl=1 2169w\" sizes=\"auto, (max-width: 723px) 100vw, 723px\" \/><figcaption class=\"wp-element-caption\">Figure 10. Forecasted snowfall (mm\/day; shading) from 05 Dec to 09 Dec 2025. The forecasts are from the 00Z 24 Nov 2025 GFS ensemble.<\/figcaption><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">Illustration by Eleanor Lutz shows Earth\u2019s seasonal climate changes. If played in full screen, the four corners present views from top, bottom and sides. It is a visual representation of scientific datasets measuring ice and snow extents.<\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter\"><img data-recalc-dims=\"1\" decoding=\"async\" src=\"https:\/\/i0.wp.com\/tabletopwhale.com\/img\/posts\/19-07-08.gif?w=723&#038;ssl=1\" alt=\"\"\/><\/figure>\n<\/div>\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n","protected":false},"excerpt":{"rendered":"<p>The polar vortex is pronounced this year, resulting in warmer temperature over the Arctic ocean, and slowing the normal sea ice recovery.\u00a0 Dr. Judah Cohen at\u00a0AER Arctic Oscillation\u00a0blog provides information like the chart above.<\/p>\n","protected":false},"author":121246920,"featured_media":415657,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_coblocks_attr":"","_coblocks_dimensions":"","_coblocks_responsive_height":"","_coblocks_accordion_ie_support":"","_crdt_document":"","advanced_seo_description":"","jetpack_seo_html_title":"Arctic Sea Ice Recovery Slows: Insights from November 2025","jetpack_seo_noindex":false,"_jetpack_newsletter_access":"","_jetpack_dont_email_post_to_subs":false,"_jetpack_newsletter_tier_id":0,"_jetpack_memberships_contains_paywalled_content":false,"_jetpack_memberships_contains_paid_content":false,"footnotes":"","jetpack_publicize_message":"","jetpack_publicize_feature_enabled":true,"jetpack_social_post_already_shared":false,"jetpack_social_options":{"image_generator_settings":{"template":"highway","default_image_id":0,"font":"","enabled":true,"token":"eyJpbWciOiJodHRwczpcL1wvaTAud3AuY29tXC9jbGltYXRlLXNjaWVuY2UucHJlc3NcL3dwLWNvbnRlbnRcL3VwbG9hZHNcLzIwMjVcLzEyXC8wQVFOTUp0WERrUjFzT3NORV9CdlU0NHlLdW9CYVlFTHZKRmNNamdHQ1hkZDVOaDU4enVvN29tS3hoQVhmb1hHb1d3N1hjWThnSzZRd0JUSXE1VXR3d1VkZlNTSEJGbzJTajRFQ19HZXVrLXpmOWNXMlJLZEFUQzRkQkNaTElMOC0xLmpwZWc_Zml0PTcyMyUyQzQwNiZzc2w9MSIsInR4dCI6IlR3byBIb3QgU3BvdHMgU2xvdyBBcmN0aWMgSWNlIFJlY292ZXJ5IE5vdmVtYmVyXHUwMGEwMjAyNSIsInRlbXBsYXRlIjoiaGlnaHdheSIsImZvbnQiOiIiLCJibG9nX2lkIjoxNTU4MTI0NDl9.zLuX60BVPRRxfr76hut7gC31B1G2cjbD2dNLkhsiT5QMQ"},"version":2},"jetpack_post_was_ever_published":false},"categories":[1],"tags":[691819671,691839930,691839929,691821637],"class_list":{"0":"post-415643","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","6":"hentry","7":"category-uncategorized","8":"tag-arctic-ice","9":"tag-arctic-oscillation","10":"tag-november-2025","11":"tag-polar-vortex","13":"fallback-thumbnail"},"jetpack_publicize_connections":[],"jetpack_featured_media_url":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/12\/0AQNMJtXDkR1sOsNE_BvU44yKuoBaYELvJFcMjgGCXdd5Nh58zuo7omKxhAXfoXGoWw7XcY8gK6QwBTIq5UtwwUdfSSHBFo2Sj4EC_Geuk-zf9cW2RKdATC4dBCZLIL8-1.jpeg?fit=1543%2C866&ssl=1","jetpack_likes_enabled":true,"jetpack_sharing_enabled":true,"jetpack_shortlink":"https:\/\/wp.me\/paxLW1-1K7V","jetpack-related-posts":[{"id":363524,"url":"https:\/\/climatescience.press\/?p=363524","url_meta":{"origin":415643,"position":0},"title":"No USA Today, Associated Press, and Others, Record Cold and Snowfall in the United States Aren\u2019t Caused by Climate Change","author":"uwe.roland.gross","date":"26\/01\/2025","format":false,"excerpt":"Lately, a series of mainstream news outlets, including USA Today, AP News, BBC Future, and Fast Company, have churned out articles claiming that January 2025\u2019s record cold and heavy snowfall across the United States are to greater or lesser degrees due to climate change, or at least that such a\u2026","rel":"","context":"In \"Associated Press\"","block_context":{"text":"Associated Press","link":"https:\/\/climatescience.press\/?tag=associated-press"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/01\/0polar-vortex-132409047_m.jpg?fit=1200%2C1067&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/01\/0polar-vortex-132409047_m.jpg?fit=1200%2C1067&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/01\/0polar-vortex-132409047_m.jpg?fit=1200%2C1067&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/01\/0polar-vortex-132409047_m.jpg?fit=1200%2C1067&ssl=1&resize=700%2C400 2x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/01\/0polar-vortex-132409047_m.jpg?fit=1200%2C1067&ssl=1&resize=1050%2C600 3x"},"classes":[]},{"id":389931,"url":"https:\/\/climatescience.press\/?p=389931","url_meta":{"origin":415643,"position":1},"title":"Climate Oscillations 9: Arctic &amp; North Atlantic Oscillations","author":"uwe.roland.gross","date":"20\/07\/2025","format":false,"excerpt":"The Arctic Oscillation (AO) is also called the Northern Annular Mode or NAM. It is analogous to the Southern Annular Mode or SAM discussed in\u00a0Climate Oscillations 5. However, there is a large difference, whereas SAM is an oscillation over an ocean that surrounds land, NAM is an oscillation over land\u2026","rel":"","context":"In \"Arctic Oscillation (AO)\"","block_context":{"text":"Arctic Oscillation (AO)","link":"https:\/\/climatescience.press\/?tag=arctic-oscillation-ao"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/07\/0figure-3.jpg?fit=1200%2C1029&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/07\/0figure-3.jpg?fit=1200%2C1029&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/07\/0figure-3.jpg?fit=1200%2C1029&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/07\/0figure-3.jpg?fit=1200%2C1029&ssl=1&resize=700%2C400 2x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/07\/0figure-3.jpg?fit=1200%2C1029&ssl=1&resize=1050%2C600 3x"},"classes":[]},{"id":384955,"url":"https:\/\/climatescience.press\/?p=384955","url_meta":{"origin":415643,"position":2},"title":"Climate Oscillations 3: Northern Hemisphere Sea Ice Area","author":"uwe.roland.gross","date":"25\/06\/2025","format":false,"excerpt":"Northern Hemisphere sea ice area is an important climatic indicator because it determines how much of the Arctic Ocean and surrounding seas are open to the atmosphere. Ice is a good insulator and traps heat in the water below it (Peixoto & Oort, 1992, p. 361). Ice is also a\u2026","rel":"","context":"In \"Arctic Oscillation (AO)\"","block_context":{"text":"Arctic Oscillation (AO)","link":"https:\/\/climatescience.press\/?tag=arctic-oscillation-ao"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/0Screenshot-2025-06-25-140141.png?fit=1200%2C766&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/0Screenshot-2025-06-25-140141.png?fit=1200%2C766&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/0Screenshot-2025-06-25-140141.png?fit=1200%2C766&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/0Screenshot-2025-06-25-140141.png?fit=1200%2C766&ssl=1&resize=700%2C400 2x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/0Screenshot-2025-06-25-140141.png?fit=1200%2C766&ssl=1&resize=1050%2C600 3x"},"classes":[]},{"id":429192,"url":"https:\/\/climatescience.press\/?p=429192","url_meta":{"origin":415643,"position":3},"title":"Vortex Slows Arctic Ice Recovery 2026 February\u00a0End","author":"uwe.roland.gross","date":"02\/03\/2026","format":false,"excerpt":"The arctic ice extents are now reported through February 2026, early on showing rising refreezing rates bringing Arctic ice extents within 200k km2 of the 20-year average. In the last 2 weeks the wavy Polar Vortex pushed cold south and replaced it with warmer southern air. Remarkably, Arctic ice reached\u2026","rel":"","context":"In \"Arctic Ice\"","block_context":{"text":"Arctic Ice","link":"https:\/\/climatescience.press\/?tag=arctic-ice"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/03\/AQOlw1vCtEftgnOGpRXoZYk9zJ9CCP1tPbc8vZ3N9d6LU8s0fLpjuKf8zADvf3zMwtoTkRAfRcV1Yb6Zxv0foCes0opS7i6i8mz9mjC2UR_wcJgUdK6dl3eqQNILV2I.jpeg?fit=1200%2C675&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/03\/AQOlw1vCtEftgnOGpRXoZYk9zJ9CCP1tPbc8vZ3N9d6LU8s0fLpjuKf8zADvf3zMwtoTkRAfRcV1Yb6Zxv0foCes0opS7i6i8mz9mjC2UR_wcJgUdK6dl3eqQNILV2I.jpeg?fit=1200%2C675&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/03\/AQOlw1vCtEftgnOGpRXoZYk9zJ9CCP1tPbc8vZ3N9d6LU8s0fLpjuKf8zADvf3zMwtoTkRAfRcV1Yb6Zxv0foCes0opS7i6i8mz9mjC2UR_wcJgUdK6dl3eqQNILV2I.jpeg?fit=1200%2C675&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/03\/AQOlw1vCtEftgnOGpRXoZYk9zJ9CCP1tPbc8vZ3N9d6LU8s0fLpjuKf8zADvf3zMwtoTkRAfRcV1Yb6Zxv0foCes0opS7i6i8mz9mjC2UR_wcJgUdK6dl3eqQNILV2I.jpeg?fit=1200%2C675&ssl=1&resize=700%2C400 2x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/03\/AQOlw1vCtEftgnOGpRXoZYk9zJ9CCP1tPbc8vZ3N9d6LU8s0fLpjuKf8zADvf3zMwtoTkRAfRcV1Yb6Zxv0foCes0opS7i6i8mz9mjC2UR_wcJgUdK6dl3eqQNILV2I.jpeg?fit=1200%2C675&ssl=1&resize=1050%2C600 3x"},"classes":[]},{"id":437132,"url":"https:\/\/climatescience.press\/?p=437132","url_meta":{"origin":415643,"position":4},"title":"2026 March Arctic Ice Recovery Slowed by\u00a0Vortex","author":"uwe.roland.gross","date":"03\/04\/2026","format":false,"excerpt":"The arctic ice extents are now reported through end of March 2026, the month whose average is taken as the annual maximum. As noted previously the wavy polar vortex has hampered ice formation with incusions of warmer southern air into the Arctic circle.","rel":"","context":"In \"Arctic Circle\"","block_context":{"text":"Arctic Circle","link":"https:\/\/climatescience.press\/?tag=arctic-circle"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-2026-March-Arctic-Ice-Recovery-Slowed-by-Vortex.jpg?fit=1168%2C784&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-2026-March-Arctic-Ice-Recovery-Slowed-by-Vortex.jpg?fit=1168%2C784&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-2026-March-Arctic-Ice-Recovery-Slowed-by-Vortex.jpg?fit=1168%2C784&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-2026-March-Arctic-Ice-Recovery-Slowed-by-Vortex.jpg?fit=1168%2C784&ssl=1&resize=700%2C400 2x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-2026-March-Arctic-Ice-Recovery-Slowed-by-Vortex.jpg?fit=1168%2C784&ssl=1&resize=1050%2C600 3x"},"classes":[]},{"id":432064,"url":"https:\/\/climatescience.press\/?p=432064","url_meta":{"origin":415643,"position":5},"title":"2026 Mid March Vortex Slows Arctic Ice\u00a0Recovery","author":"uwe.roland.gross","date":"18\/03\/2026","format":false,"excerpt":"The arctic ice extents are now reported through March 16, 2026, an important date just past the annual daily maximum for Arctic ice extents averaged over the last 20 years. As noted in February, the wavy polar vortex has hampered ice formation with incusions of warmer southern air into the\u2026","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/03\/0-polar-vortex1.jpg?fit=784%2C1168&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/03\/0-polar-vortex1.jpg?fit=784%2C1168&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/03\/0-polar-vortex1.jpg?fit=784%2C1168&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/03\/0-polar-vortex1.jpg?fit=784%2C1168&ssl=1&resize=700%2C400 2x"},"classes":[]}],"_links":{"self":[{"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts\/415643","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/users\/121246920"}],"replies":[{"embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=415643"}],"version-history":[{"count":8,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts\/415643\/revisions"}],"predecessor-version":[{"id":415660,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts\/415643\/revisions\/415660"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/media\/415657"}],"wp:attachment":[{"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=415643"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=415643"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=415643"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}