Beaufort Gyre

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The Beaufort Gyre is a wind-driven ocean current located in the Arctic Ocean polar region. The gyre contains both ice and water. It accumulates fresh water by the process of melting the ice floating on the surface of the water.[1]

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[edit] Studies

The gyre has formed a dome of freshwater that has risen by about 15 centimetres (5.9 in) since 2002; by 2011 it has grown to about 8,000 cubic kilometres (1,900 cu mi) in volume.[2] The freshwater represents about 10% of all freshwater in the Arctic; it comes mostly from Russian river runoff.[2]

Oceanographer Andrey Proshutinsky has theorized that if winds and the gyre are to weaken, high volumes of freshwater could leak out of the eastern side of the Arctic Ocean. The fresh water could leak into the Northern Atlantic Ocean, causing large impacts on ocean circulation and climate.[3]

Due to ice, The Beaufort Gyre is difficult to access in the winter, and the shorter days make necessary the use of artificial light.[1] Studies by Arthur S. Dyke and others show that if rivers increased discharges into the Beaufort Gyre, it might shift it to the right.[4]

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