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)....

Full description

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: American Geophysical Union 2004
Subjects:
Online Access:https://doi.org/10.1029/2004JC002441
http://ecite.utas.edu.au/32348