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...
Published in: | Antarctic Science |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Cambridge University Press (CUP)
2003
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Online Access: | http://dx.doi.org/10.1017/s0954102003001159 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102003001159 |