Modeling water mass formation in the Mertz Glacier Polynya and Adelie Depression, East Antarctica
High rates of sea ice growth rejection in the Mertz Glacier Polynya drive the production of dense continental shelf waters in the Adlie Depression. We consider the rate of outflow of waters having sufficient density to sink into the neighboring abyssal ocean and form Adlie Land Bottom Water (ALBW)....
Published in: | Journal of Geophysical Research |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union
2004
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Subjects: | |
Online Access: | https://doi.org/10.1029/2004JC002441 http://ecite.utas.edu.au/32348 |