Abstract
A two-layer model of circulation is developed in an open-ocean basin where a vertically homogeneous layer overlays a thermoclinic region. In the latter, the temperature changes in an exponential manner to a constant abyssal value. The motions are driven by an Ekman suction and cooling (or heating) of the ocean surface....
Recommended Citation
Niiler, Pearn P., and Pieter S. Dubbelday. 1970. "Circulation in a wind-swept and cooled ocean." Journal of Marine Research 28, (2). https://elischolar.library.yale.edu/journal_of_marine_research/1179
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