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<p>In the Beaufort Gyre, free-floating sea ice, which is very mobile and susceptible to winds, drifts in a clockwise direction due to a high-pressure system that fosters anti-cyclonic winds. Historically, the sea ice drifted around the gyre for up to ten years, growing thicker and ageing into so-called multiyear ice, while accumulating snow and ice each winter. This process used to supply the Arctic with extensive multiyear sea ice coverage. Warming temperatures and increased melt in the <a href="page.php?w=Beaufort_Sea">Beaufort Sea</a> in the</p><p>
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