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.
The Labrador Sea contains bergy water. Frobisher Bay contains mostly bergy water with some old and first-year ice present at its entrance. Foxe Basin contains first-year ice with many open water areas present. Northern and eastern Baffin Bay contain bergy water while southwestern Baffin Bay contains mostly first-year ice with some old ice. Western Davis Strait contains first-year ice with some old ice, while its eastern section is bergy water.
North of Ellesmere Island contain old ice with some first-year ice. Nares Strait comprises old and first-year ice in roughly equal proportion. Eureka Sound contain first-year ice with low amounts of old ice. The ice in Jones Sound is completely mobile except for some small areas on the northern coast. Lancaster Sound is mostly bergy water. The Gulf of Boothia contains first-year ice except where a trace of old ice is present north of 71.5N. Cumberland Sound contains some old and first-year ice in its eastern section and bergy water in its western section.
Canada Basin comprises old ice with some first-year ice. The Beaufort Sea contains an even mixture of old and first-year ice. First-year ice is only present along the coastline of Alaska, Yukon and the Northwest Territories. Amundsen Gulf contains mostly first-year ice with low amounts of old ice. Coronation Gulf contains bergy water. Queen Maud Gulf is bergy water with some first-year ice in the northern sections. M’Clintock Channel and Peel Sound comprise mobile first-year ice with a trace of old ice. Barrow Strait contains mobile first-year ice with a trace of old ice in its eastern section, while its western section contains a mixture of old and first-year ice. Ice in M’Clure Strait is entirely mobile with an even mixture of old and first-year ice. The Queen Elizabeth Islands remains fast except for Norwegian Bay. Mobile and fasted ice comprise a mixture of old ice and first-year ice.
James Bay is ice free. Northern and central Hudson Bay are ice free. Southern Hudson Bay consists mostly of open water with an area of first-year ice present along the western shoreline. Some first-year ice is present in the extreme northwestern section of Hudson Strait. Otherwise, Hudson Strait and Ungava Bay consists of bergy water.
The pack ice edge in the northern Kara Sea has retreated up to 90 NM eastward as a result of melting and movement due to winds. The fast ice along the mainland Russian coast has weakened and become entirely mobile, while the fast ice along Severnaya Zemlya has reduced, but remains fasted in more sheltered areas. In the southern Kara Sea, ice remains only in the vicinity of the southern portion of Novaya Zemlya, 8 NM from the coast at the closest point.