Modeling water mass formation in the Mertz Glacier Polynya and Adelie Depression, East Antarctica

High rates of sea ice growth and brine rejection in the Mertz Glacier Polynya drive the production of dense continental shelf waters in the Adelie Depression. We consider the rate of outflow of waters having sufficient density to sink into the neighboring abyssal ocean and form Adelie Land Bottom Wa...

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Bibliographic Details
Published in:Journal of Geophysical Research
Main Authors: Marsland, S., Bindoff, N., Williams, G., Budd, W.
Format: Article in Journal/Newspaper
Language:English
Published: 2004
Subjects:
Online Access:http://hdl.handle.net/11858/00-001M-0000-0011-FFDF-9
http://hdl.handle.net/11858/00-001M-0000-0011-FFDE-B