Circulation in the Eastern Bering Sea: Inferences from a 2-km-resolution model
A 2-km-resolution model of the eastern Bering Sea is developed to capture dynamical processes on the scale of the Rossby radius of deformation on tidal to seasonal time scales. The model spans the region from 178°E to the Alaskan coast and from roughly 50° to 66°N, including the Aleutian Islands in...
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Veröffentlicht in: | Deep-sea research. Part II, Topical studies in oceanography Topical studies in oceanography, 2016-12, Vol.134, p.48-64 |
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Sprache: | eng |
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