A Theory of Water Percolation in Snow

Abstract A theory is developed to describe the vertical percolation of water in isothermal snow. The general theory of Darcian flow is reviewed to establish a reasonable physical basis for the construction of a model. It is shown that in simple gravity drainage, capillarity is negligible compared wi...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Colbeck, S. C.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1972
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000022346
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000022346