Regional charts and associated synopsis write-up capture ice and environmental conditions throughout the Arctic which are based on the U.S. National Ice Center’s weekly analysis. Charts and synopses are updated weekly on Fridays. Note: Baltic Sea analysis is provided by the Finnish Meteorological Institute. The Canadian Archipelago (Canada East, Canada North, Canada West, and Hudson Bay) analysis is provided by the Canadian Ice Service.
Eastern Canada Basin contains multi-year ice with some second-year ice. Greely Fjord and Eureka Sound contain some multi-year ice and second-year ice, with new and young ice continuing to develop. Jones Sound comprises of primarily young ice with some multi-year ice and second-year ice. Some new and young ice is present along the coastal areas of Greenland. Davis Strait, Cumberland Sound, and the Labrador Sea contain bergy water. Frobisher Bay has new ice forming near Iqaluit.
Nares Strait contains multi-year ice with some second-year ice. New and young ice continues to develop throughout the ice pack. Some thin first year fast ice now exists in the northernmost fjords of Ellesmere Island. Multi-year ice is descending southwards into Baffin Bay to 73.5N. Gulf of Boothia is mostly bergy water in southern half and contains new ice, young ice and some multi-year ice northern section.
Canada Basin comprises mostly multi-year ice with some second-year ice in the eastern section, transitioning to mainly second-year ice with some multi-year ice westwards. Young ice and new ice cover much of the southwest extent. The Beaufort Sea contains a mix of multi-year ice, second-year ice, young ice and new ice. New ice is developing along the coasts. The channels in and around the Queen Elizabeth Islands comprise mostly multi-year ice with some second-year ice. New ice and young ice continue to develop where the ice pack has moved away from the coast, particularly along the eastern shores of the islands. M’Clure Strait contains a very close pack of multi-year ice. Viscount Melville Sound and Barrow Strait contain a close pack composed mainly of multi-year ice, with some second-year and young ice. South of Cornwallis Island, a very close pack consists primarily of young and new ice, with some multi-year and second-year ice. M’Clintock Channel contains a very close to close pack of mixed multi-year, second-year, young, and new ice. Peel Sound contains mostly new ice and small amounts of grey ice with multi-year ice present in the northern section. Queen Maud Gulf is bergy water with new ice developing along the coast. Coronation Gulf and Amundsen Gulf are mostly bergy water except where new ice is developing along the southern coast. Barrow Strait and western Lancaster Sound contain multi-year ice, young ice and new ice.
Decreasing air temperatures across the Chukchi Sea allowed for the ice edge to expand anywhere from 30 to 80 NM. New ice is beginning to develop along the Alaskan and Russian coasts, particularly in Kotzebue Sound and in vicinity of Utqiagvik. Analysis confidence: High- complete SAR coverage over AOI.
Steady ice growth continued across the Laptev Sea. The location of the ice edge did not change significantly, however, ice at the edge developed and increased in concentration. Ice growth accelerated along the coastline, with much of the eastern and central coast now covered in 10 - 50 NM of new and young ice. Analysis confidence: High - complete SAR coverage over AOI.