Author:
Banke E. G.,Smith S. D.,Anderson R. J.
Abstract
Eddy flux measurements of wind stress on the arctic pack ice have been made in summer and winter in terrain ranging from fiat to hummocked. Parameterization by a drag coefficient dependent on a surface parameter is suggested. Reduced values of the drag coefficient were observed in highly stable stratification. The coefficient for sensible heat flux is lower than the drag coefficient. Wind drag on ice ridges has been measured by a pressure differential method.
Publisher
Canadian Science Publishing
Cited by
40 articles.
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