Journal of the Meteorological Society of Japan. Ser. II
Online ISSN : 2186-9057
Print ISSN : 0026-1165
ISSN-L : 0026-1165
On the Mechanism of Thaw Water Movement in Snow Deposit
R. Saitô
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1941 Volume 19 Issue 4 Pages 153-156

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Abstract
According to the author's observations, it is more plausible that downward movement of thaw water in snow is acsribed to connection of water films covering snow particles, rather than that it is caused by capillary attraction of water.
The velocity of downward movement of thaw water does not depend on the specific gravity of snow. but on the size of snow grains. This is explained without difficulty by the water film theory, which is also powerful for explanation of “leader” (water stream) formation.
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