Is thermobaricity a major factor in Southern Ocean ventilation?

The Weddell Polynya, a large expanse of water that originated over Maud Rise (a bathymetric protrusion centred near 64°30′S, 3°E) and remained open during winter in the late 1970s, may have manifested a mode of deep ocean convection where despite large heat loss at the surface, sustained heat transp...

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Bibliographic Details
Published in:Antarctic Science
Main Author: MCPHEE, MILES G.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2003
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102003001159
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102003001159