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.
Nares Strait is comprised of multi-year ice with some second-year ice. New and young continue to develop throughout the icepack. Multi-year ice continues to expand southwards into Baffin Bay to 75N. Nansen Sound contains multi-year ice and second year ice. Greely Fjord and Eureka Sound contain some multi-year ice and second-year ice with new and young ice continuing to form. The ice in and around Queen Elizabeth Islands is mostly multi-year, with some second-year ice present. New and young ice continue to develop throughout the area.
The pack ice in Canada Basin consists mainly of multi-year ice with some second year ice in its eastern section and second year ice with some multi-year ice in its western section. Young ice and new ice are covering most of the western extent. The Beaufort Sea contains multi-year, second year, and young ice in open drift and close pack conditions. Areas of bergy water remain in the southern section with new ice covering most of the coastal area. The channels in and around the Queen Elizabeth Islands contain mostly multi-year ice, with some second year ice. New ice and young ice are covering areas where the pack ice has moved away from the coasts, particularly along the southern coast of the islands. M’Clure Strait contains mostly multi-year ice, with some second year ice present in very close pack conditions. The previously open drift of mostly multi-year and second year ice has persisted in Viscount Melville Sound and Barrow Strait, while the intervening areas have filled with new ice. Widespread areas of new ice forming in the region south of Bathurst Island. The area south of Cornwallis Island is covered with a mix of close pack multi-year, second year and new ice and bergy water. M’Clintock Channel contains a mix of multi-year ice and second year ice with some new ice forming between the floes in mostly close pack conditions except for the southeastern section of the channel where bergy water was still present. Peel Sound is mostly bergy water with very open drift multi-year, second year and new ice in the northwestern section of the sound. Coronation Gulf, Amundsen Gulf, and Queen Maud Gulf are bergy water.
Abundant new ice development has occurred in the Laptev Sea due to below freezing air temperatures, 0°C to -14°C. New ice growth is evident along the Russian coastline and the pack ice edge, decreasing the open water along the Northern Sea Route. Analysis confidence: High - total SAR coverage of sea ice within the Laptev Sea