Abstract
The effect of cooling on the separated boundary current predicted by the model of Parsons is studied. The separating current is found to strengthen and to move southwards and eastwards. The model is also robust to limited heating, in which case the separating current weakens and moves northwards. © 1990 American Meteorological Society.
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CITATION STYLE
APA
Nurser, A. J. G., & Williams, R. G. (1990). Cooling parsons’ model of the separated gulf stream. Journal of Physical Oceanography, 20(12), 1974–1979. https://doi.org/10.1175/1520-0485(1990)020<1974:CPMOTS>2.0.CO;2
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