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
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.494.3747 |