Hudson Bay High Sea
Southern Hudson Bay is a shallow expanse of cold water, fed by rivers draining the surrounding lowlands. Wind and river runoff help drive a broad counterclockwise circulation around the bay, whose waters ultimately leave through Hudson Strait. For much of the year the surface is covered with ice. Ships serving the fur-trading posts depended on the short season of open water; if ice blocked their return through the strait, their crews could be forced to winter on the bay.
References
- www.canada.ca/en/canadian-coast-guard/corporate/publications/ice-navigation-in-canadian-waters/chapter-3-ice-climatology-environmental-conditions.html
- waves-vagues.dfo-mpo.gc.ca/Library/314704ch5.pdf
- pame.is/images/03_Projects/AMSA/AMSA_Background_Research_Docs/History_and_Governance_of_Arctic_Shipping/2-2-Early-Arctic-Marine-Transport-History.pdf