Arctic sea ice continued the fast retreat that was observed in July through August 10, followed by a brief slowdown, only to pick up pace again. During the first half of August, the ice primarily retreated in the northern Beaufort Sea and in the East Siberian Sea. The ice also mostly cleared out of the Northwest Passage, whereas ice remained in the Chukchi Sea, along the Northern Sea Route. In the Southern Ocean, sea ice began to expand rapidly after a slow growth from May through July, but remains at the second lowest daily extent as of this post.
Overview of conditions
Arctic sea ice extent as of August 18 was 5.20 million square kilometers (2.01 million square miles) (Figure 1a). The first week of August continued to have the rapid pace of ice loss observed in July (Figure 1b). However, afterwards the pace slowed for several days but picked up again. Extent approaches 2007 levels, while tracking above the record 2012 minimum. Sea ice extent is currently fourth lowest, behind 2012, 2019, and 2020.
Ice loss has primarily occurred in the northern part of the Beaufort Sea and to a lesser extent in the East Siberian Sea as well as in the Canadian Archipelago, where the Northwest Passage is nearly ice free. Elsewhere, there has been little northward retreat of the sea ice edge. The high-concentration area of ice south and east of Wrangel Island has remained, though some openings started to emerge off the coast of Siberia as southerly winds drove this packed ice northwards. Most of the remaining ice is of low ice concentration. As of August 18, the sea ice extent was 1.98 million square kilometers (764,000 square miles) below the 1981 to 2010 average and 540,000 square kilometers (208,000 square miles) above 2012, the record low for this time of year.
Conditions in context
Although ice loss during the first half of August was faster than average, air temperatures at the 925 hPa level (approximately 2,500 feet above the surface) were 2 to 4 degrees Celsius (4 to 7 degrees Fahrenheit) below average over much of the Arctic Ocean, stretching from the coast of Siberia across the pole towards northern Greenland (Figure 2a). Above average air temperatures were mostly recorded in the East Greenland, Barents, and Kara Seas, as well as in the southern Beaufort Sea and the Canadian Arctic Archipelago. Air temperatures in the Barents Sea near Franz Joseph Land were as much as 8 degrees Celsius (14 degrees Fahrenheit) above average where a strong anticyclone (high sea level pressure) was located (Figure 2b). Low sea level pressure dominated the Chukchi and East Siberian Seas. Coupled with the high pressure over eastern North America, warm winds from the south moved into the Beaufort Sea while cold air from the Arctic Ocean moved into the Chukchi Sea.
Summer came early to the Arctic
Little sea ice in the Northwest Passage routes
Historically, the presence of multiyear sea ice has stymied visions of the NWP becoming a trade route, but recent reductions in sea ice caused by climate change are reinvigorating these visions. A recent study by Alison Cook and colleagues reviewed four possible routes through the NWP and considered ships with different levels of ice strengthening over the past 15 years (Figure 4c). The study found that sea ice frequently obstructed some areas of the NWP leading to consistently shortened shipping seasons over the past 15 years. Despite the shipping season length becoming longer in several other sections of the NWP, the viability of full passage is actually lessening as a consequence of climate change. This finding is linked to sea ice melting in the Arctic Ocean between northern Greenland and the Canadian Archipelago, often referred to as the Last Ice Area, which is breaking up and migrating south, clogging narrow channels in the NWP and hampering route reliability for ships operating in the region. These results support those from an earlier study this year by Stephen Howell and colleagues.
Wildfires in the north
Arctic minimum projection
As noted above, currently, the sea ice extent stands at fourth lowest for this time of year. We can estimate the extent through the end of the summer using the daily ice loss rates from previous years to project the September minimum extent. This method, which has been regularly contributed to the Sea Ice Outlook, provides a reasonable range of the minimum extent. This year, using the average daily loss rates from 2007 to 2023, the projection starting from August 18 results in a projected minimum of 4.14 million square kilometers (1.60 million square miles), with a range of 3.93 to 4.35 million square kilometers (1.52 to 1.68 million square miles) (Figure 6). This suggests that this year’s minimum will potentially be the third lowest in the satellite record and likely to fall somewhere between the second and eighth lowest. It indicates that a new record low surpassing 2012 is very unlikely.
Rapid autumn ice growth down under
After slow growth from May through July, Antarctic sea ice has started to rapidly expand since the beginning of August. The growth has primarily occurred in the Weddell Sea and to a lesser extent in the Indian and Pacific Oceans (Figure 7). Ice growth for the first two weeks of August was 1.5 million square kilometers (580,000 square miles) per day, among the fastest ice growth rates seen in the 46-year record for this time of year. Nevertheless, the total extent remained the second lowest in the satellite data record. As of August 18, the extent was 1.27 million square kilometers (490,000 square miles) below the 1981 to 2010 average, and 1.07 million square kilometers (413,000 square miles) above 2023.
Further reading
Cook, A. J., J. Dawson, S. E. L. Howell, J. E. Halloway, and M. Brady. 2024. Sea ice choke points reduce the length of the shipping season in the Northwest Passage, Communications Earth & Environment, 5, 362, doi.org:10.1038/s43247-024-01477-6.
Howell, S. E. L., D. G. Babb, J. C. Landy, I. A. Glissenaar, K. McNeil, B. Montpetit, and M. Brady. 2024. Sea ice transport and replenishment across and within the Canadian Arctic Archipelago, 2016–2022. The Cryosphere, 18, 2321–2333, doi.10.5194/tc-18-2321-2024.