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Bering Slope Current

The eastern part of the subpolar gyre in the deep (western) part of the Bering Sea. Currents in this gyre are weak (0. 1ā€“0. 2 m sāˆ’1) but reach to the ocean floor and are associated with eddy formation at oceanic ridges. A southward countercurrent with maximum speeds of 0. 25 m sāˆ’1 near a depth of 150 m exists between the shelf and the northward-flowing Bering Slope Current, indicating its character as the eastern boundary current of a subpolar gyre.

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Penulis

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