Abstract
During a synoptic hydrocast survey in September 1993 near the Aleutian Islands, net northward flow of Alaskan Stream water occurred through deep passes near 180 and 172W. This inflow (≈4 × 106 m3 s−1) was the source of the eastward flow in the Bering Sea north of the islands. The eastward flow, however, was weaker and more convoluted than the stream flow (≈7 × 106 m3 s−1, referred to 1000 db) south of the islands.
Recommended Citation
Reed, R. K., and P. J. Stabeno. 1994. "Flow along and across the Aleutian Ridge." Journal of Marine Research 52, (4). https://elischolar.library.yale.edu/journal_of_marine_research/2108
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