Study Area (IMAGE) University of Washington Caption The Beaufort Gyre is a clockwise wind pattern in the western Arctic Ocean that causes freshwater to accumulate at the ocean's surface. When those winds relax, the freshwater drains not through Fram Strait, but through the narrow channels of the Canadian Archipelago to reach the Labrador Sea, off the coast of Canada's Newfoundland and Labrador. Credit University of Washington Usage Restrictions With credit License Licensed content Disclaimer: AAAS and EurekAlert! are not responsible for the accuracy of news releases posted to EurekAlert! by contributing institutions or for the use of any information through the EurekAlert system.