Abstract
Based on a limited set of available oxygen isotope measurements, it is hypothesized that the mean now in the Middle Atlantic Bight is part of a 5000 km-long buoyancy-driven, coastal current which originates along the southern coast of Greenland. This idea is consistent with most features of the known circulation of the region.
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CITATION STYLE
APA
Chapman, D. C., & Beardsley, R. C. (1989). On the Origin of Shelf Water in the Middle Atlantic Bight. Journal of Physical Oceanography, 19(3), 384–391. https://doi.org/10.1175/1520-0485(1989)019<0384:otoosw>2.0.co;2
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