Seasonal variations in drag coefficient over a Sastrugi-covered snowfield in coastal East Antarctica

The surface of windy Antarctic snowfields is subject to drifting snow, which leads to the formation of sastrugi. In turn, sastrugi contribute to the drag exerted by the snowsurface on the atmosphere and hence influence drifting snow. Although the surface drag over rough sastrugi fields has been esti...

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Bibliographic Details
Published in:Boundary-Layer Meteorology
Main Authors: Amory, C., Gallee, H., Naaim-Bouvet, F., Favier, V., Vignon, E., Picard, G., Trouvilliez, A., Piard, L., Genthon, C., Bellot, H.
Other Authors: IRD UMR 5001 IGE GRENOBLE FRA, IRSTEA GRENOBLE UR ETGR FRA
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:https://irsteadoc.irstea.fr/cemoa/PUB00057155