14A.6 CASE STUDIES OF KATABATIC WIND IN COATS LAND, ANTARCTICA

The ice cap of Antarctica loses heat due to radiative cooling at the surface, which then cools the overlying atmospheric boundary layer. The resulting (dense) layer of cold air will accelerate

Bibliographic Details
Main Authors: Hanneke Luijting, Ian A. Renfrew, Philip S. Anderson, John C. King
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Coats Land
Antarc*
Antarctica
Ice cap
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.494.3747
Description
Summary:The ice cap of Antarctica loses heat due to radiative cooling at the surface, which then cools the overlying atmospheric boundary layer. The resulting (dense) layer of cold air will accelerate

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