{"id":436,"date":"2023-05-17T07:24:53","date_gmt":"2023-05-17T07:24:53","guid":{"rendered":"https:\/\/arcticwatch.info\/index.php\/2023\/05\/17\/facts-about-the-arctic-in-may-2023\/"},"modified":"2025-07-14T01:00:58","modified_gmt":"2025-07-13T23:00:58","slug":"facts-about-the-arctic-in-may-2023","status":"publish","type":"post","link":"https:\/\/arcticwatch.info\/index.php\/2023\/05\/17\/facts-about-the-arctic-in-may-2023\/","title":{"rendered":"Facts About the Arctic in May 2023"},"content":{"rendered":"
\n

At the beginning of May AWI\u2019s high resolution AMSR2 extent<\/a> metric is at the top of the historical range:<\/p>\n

\"\"<\/a><\/figure>\n

After a period of melt in the East Greenland Sea, export of sea ice from the Central Arctic via the Fram Strait has increased recently:<\/p>\n

\"\"<\/a><\/figure>\n

Sea ice area in the Barents Sea peaked in the first week of April and has declined steadily since then:<\/p>\n

\"\"<\/a><\/figure>\n

SMOS data<\/a> is flowing again, and the gaps have been filled. Here\u2019s the final pre melt ponding map of the spring:<\/p>\n

\"\"<\/a><\/figure>\n

It reveals large areas of thin ice that have recently developed in the Kara Sea. Here\u2019s a pseudo colour glimpse of the region through the clouds:<\/p>\n

\"\"<\/a>
\u201cFalse colour\u201d image of the Kara Sea on May 1st<\/a>\u00a0from the MODIS instrument on the Terra satellite<\/em><\/figcaption><\/figure>\n

and the regional sea ice area graph:<\/p>\n

\"\"<\/a><\/figure>\n

An area of thin ice has also developed off the Chukchi Sea coast of Alaska.<\/p>\n

<\/a>[Edit \u2013 May 4th]<\/strong><\/p>\n

The PIOMAS gridded thickness data for April show that the 2023 maximum volume of 23,320 km<\/span>3<\/sup> was reached on April 23rd:<\/p>\n

\"\"<\/a><\/figure>\n

Here too is the thickness map for April 30th:<\/p>\n

\"\"<\/a><\/figure>\n

In Arctic weather news there is currently a cyclone spinning over the Laptev Sea which is forecast by GFS to reach a minimum MSLP of 971 hPa later today:<\/p>\n

\"\"<\/a><\/figure>\n

It remains to be seen what effect the inclement weather has on the ice in the region.<\/p>\n

<\/a>[Edit \u2013 May 5th]<\/strong><\/p>\n

As Neil points out below<\/a>, the May edition of the\u00a0NSIDC\u2019s Arctic Sea Ice News<\/a> has been published:<\/p>\n

Air temperatures at the 925 hPa level in April were near average to below average over most of the Arctic Ocean. This helps to explain the slow rate of sea ice loss during April. While temperatures were modestly above average over the Barents Sea, these areas are already largely free of sea ice:<\/p><\/blockquote>\n

\"\"<\/a><\/figure>\n

The sea level pressure pattern was characterized by fairly high pressure over most of the Arctic Ocean. The clockwise winds around a separate high-pressure center over Scandinavia brought warm winds from the south over the Barents Sea, consistent with the above air average temperatures in that area. Similarly, below-average\u00a0temperatures over Alaska were driven by the combination of a strong low pressure area in the Gulf of Alaska and high pressure in the Beaufort Sea, driving air generally southward from the ice-covered Arctic Ocean.<\/p><\/blockquote>\n

\"\"<\/a><\/figure>\n

The NSIDC article also mentions a new open access paper by Sledd et al. entitled \u201cClouds Increasingly Influence Arctic Sea Surface Temperatures as CO2<\/sub>\u00a0Rises<\/a>\u201c. Here\u2019s an extract from the abstract:<\/p>\n

Under pre-industrial CO2<\/sub>\u00a0concentrations, summer clouds have little direct effect on maximum annual sea surface temperatures (SST). When CO2<\/sub>\u00a0concentrations increase, sea ice retreats earlier, allowing more solar radiation to warm the ocean. Clouds can counteract this summer warming by reflecting solar radiation back to space. Consequently, clouds explain up to 13% more variability in maximum annual SST under modern-day CO2<\/sub>\u00a0concentrations. Maximum annual SST are three times more sensitive to summer clouds when CO2<\/sub>\u00a0concentrations are four times pre-industrial levels.<\/p><\/blockquote>\n

<\/a>[Edit \u2013 May 7th]<\/strong><\/p>\n

Since Neil is wondering about the recent \u201cslow melt\u201d, here\u2019s an animation of Arctic sea ice drift over the last month. Click the image if your bandwidth supports viewing a 13 Mb video:<\/p>\n

\"\"<\/a>
Click to animate (13 Mb!)<\/em><\/figcaption><\/figure>\n

<\/a>[Edit \u2013 May 11th]<\/strong><\/p>\n

Melt ponds (and a patch of open water) are now clearly visible along the coast of the Coronation Gulf in the Canadian Arctic Archipelago:<\/p>\n

\"\"<\/a>
\u201cFalse colour\u201d image of the Coronation Gulf on May 11th<\/a>\u00a0from the MODIS instrument on the Terra satellite<\/em><\/figcaption><\/figure>\n

The Swedish icebreaker Oden is now in the marginal ice zone west of Svalbard. It won\u2019t come as a surprise to regular readers that the Art of Melt 2023 expedition blog reports<\/a> that:<\/p>\n

We encountered the first ice on the first day, which quickly became quite challenging to break, even for Oden, as there were many ridges and bumps on the ice.<\/p><\/blockquote>\n

\"\"<\/a><\/figure>\n

<\/a>[Edit \u2013 May 13th]<\/strong><\/p>\n

Above zero temperatures are forecast<\/a> for the Beaufort Sea by the end of the weekend:<\/p>\n

\"\"<\/a><\/figure>\n

The weather is already warm in the Canadian Arctic Archipelago. Here\u2019s the report from Kugluktuk<\/a> for the last 24 hours:<\/p>\n

\"\"<\/a><\/figure>\n

Melt ponds are now visible in Franklin and Darnley Bays:<\/p>\n

\"\"<\/a>
\u201cFalse colour\u201d image of the Amundsen Gulf on May 12th<\/a>\u00a0from the MODIS instrument on the Aqua satellite<\/em><\/figcaption><\/figure>\n

<\/a>[Edit \u2013 May 15th]<\/strong><\/p>\n

Melt ponds are now visible in the Beaufort Sea off the Mackenzie Delta:<\/p>\n

\"\"<\/a>
\u201cFalse colour\u201d image of the Mackenzie Delta on May 15th<\/a>\u00a0from the MODIS instrument on the Terra satellite<\/em><\/figcaption><\/figure>\n

Watch this space!<\/p>\n<\/div>\n","protected":false},"excerpt":{"rendered":"

At the beginning of May AWI\u2019s high resolution AMSR2 extent metric is at the top of the historical range.<\/p>\n","protected":false},"author":2,"featured_media":437,"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":[4],"tags":[],"class_list":["post-436","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-analysis"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/posts\/436","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=436"}],"version-history":[{"count":1,"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/posts\/436\/revisions"}],"predecessor-version":[{"id":3259,"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/posts\/436\/revisions\/3259"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/media\/437"}],"wp:attachment":[{"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/media?parent=436"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/categories?post=436"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/arcticwatch.info\/index.php\/wp-json\/wp\/v2\/tags?post=436"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}