Abstract
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland Ridge and have water properties that suggest an origin near the Tail of the Bank. The eddies appear to be important features of the circulation over the Ridge....
Recommended Citation
Mountain, D. G., and J. L. Shuhy. 1980. "Circulation near the Newfoundland Ridge." Journal of Marine Research 38, (2). https://elischolar.library.yale.edu/journal_of_marine_research/1507
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