
Russian Nuclear Icebreakers on the Northern Sea Route, March 2025
The arctic ice extents are now reported through mid-July 2026, and as noted previously the wavy polar vortex has hampered ice formation with incursions of warmer southern air into the Arctic circle. This factor receded in May and June, with extents closing the gap with the averages. The Northern Sea Route (NSR) goes through the Russian shelf seas of Laptev, East Siberian, and Chukchi seas on the way to Bering Strait in Beaufort Sea.
As the image from July 15 shows, despite the melting on the margins, the Arctic Ocean core is solid, expecially along the Eurasian NSR seen on the left vertical side. Some open water is appearing in Laptev (top left) and East Siberian sea (mid Left), but still extensive land fast ice. As usual mid July, Hudson Bay (bottom right) is mostly open water, as is Baffin Bay (middle right). Canadain Archipelago remains largely ice covered.
The chart below shows the 20-year mid July averages for Arctic ice extents, along with 2026, 2025 and 2007 as well as SII v.4. Note that on average during this period 2.4M km2 of ice extent is lost. By comparison SII v.4 lost 2.6M and MASIE lost 2.2M. In other words, MASIE 2026 ice melt is just one day ahead of average.
Note the deficit to average mid-June was ~400k km2 but since then 2026 extents tracked close to average before ending down 110k km2. SII tracked close to MASIE last half of June, but as we have seen in previous months SII v.4 lost a lot of ice in the last two weeks ending 338k km2 lower than MASIE, or 1/3 of a Wadham.
The table below shows the distibution of ice extents on day 196 across regions of the Arctic ocean.
| Region | 2026196 | Day 196 Average | 2026-Ave. | 2007196 | 2026-2007 |
| (0) Northern_Hemisphere | 8230702 | 8340811 | -110110 | 8354527 | -123825 |
| (1) Beaufort_Sea | 1044469 | 874320 | 170149 | 845938 | 198531 |
| (2) Chukchi_Sea | 781718 | 647606 | 134112 | 576079 | 205639 |
| (3) East_Siberian_Sea | 908640 | 924076 | -15436 | 788128 | 120513 |
| (4) Laptev_Sea | 719818 | 563593 | 156224 | 575520 | 144298 |
| (5) Kara_Sea | 245022 | 350290 | -105268 | 483785 | -238762 |
| (6) Barents_Sea | 36 | 53993 | -53957 | 75731 | -75695 |
| (7) Greenland_Sea | 321463 | 401993 | -80531 | 472890 | -151428 |
| (8) Baffin_Bay_Gulf_of_St._Lawrence | 267821 | 309518 | -41696 | 342503 | -74682 |
| (9) Canadian_Archipelago | 719994 | 707260 | 12734 | 730894 | -10900 |
| (10) Hudson_Bay | 184771 | 339584 | -154813 | 248785 | -64014 |
| (11) Central_Arctic | 3034736 | 3164687 | -129951 | 3211275 | -176539 |
The table shows that many regions are close to or above the 20-year average. The Eurasian shelf seas of Laptev, Chukchi and Beaufort are in surplus. The majority of the 1.3% overall deficit is from Hudson Bay, Central Arctic, Kara and Greenland seas. Excepting Central Arctic, those regions will be ice-free end of summer. Bering and Okhotsk seas are left off the list since they are open water now as usual.


Illustration by Eleanor Lutz shows Earth’s 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.


