Vertical Circulation Off the Ross Ice Shelf

ABSTRACT: The Ross Ice Shelf is a floating ice mass about 200m thick over an average depth along the barrier of 567 m. In January the prevailing wind blows. from the east, parallel to the coast. The wind current transports the low saliniry layer (ca. 50 m) toward the ice shelf, where it must descend...

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Bibliographic Details
Main Author: C. W. Thomas
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1965
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.504.5320
http://scholarspace.manoa.hawaii.edu/bitstream/handle/10125/7756/vol20n2-239-245.pdf;jsessionid=25FD059843F6196CD1E03054D89EA376?sequence=1