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Kamchatka Current

From Wikipedia, the free encyclopedia

The Kamchatka Current is a cold-water current flowing southwestward in the Bering Sea, along the Siberian Kamchatka Peninsula. It receives water from the Bering Slope Current.[1] A portion of this current then becomes the Oyashio Current while the remainder joins the warmer North Pacific Current.

See also

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References

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  1. ^ "Surface circulation of the Bering Sea (schematically)".