Modeling water mass formation in the Mertz Glacier Polynya and Ade´lie 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 Ade´lie Depression. We consider the rate of outflow of waters having sufficient density to sink into the neighboring abyssal ocean and form Ade´lie Land Bottom...

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Bibliographic Details
Published in:Journal of Geophysical Research
Main Authors: Marsland, SJ, Bindoff, NL, Williams, GD, Budd, WF
Format: Article in Journal/Newspaper
Language:English
Published: 2004
Subjects:
Online Access:https://eprints.utas.edu.au/6378/
https://eprints.utas.edu.au/6378/1/Marsland_Bindoff_Williams_Budd_2004.pdf
https://doi.org/10.1029/2004JC002441