WATER-FLOW THROUGH HETEROGENEOUS SNOW

被引：70

作者：

COLBECK, SC

机构：

[1] U.S. Army Cold Regions Research and Engineering Laboratory, Hanover

来源：

COLD REGIONS SCIENCE AND TECHNOLOGY | 1979年 / 1卷 / 01期

关键词：

D O I：

10.1016/0165-232X(79)90017-X

中图分类号：

X [环境科学、安全科学];

学科分类号：

08 ; 0830 ;

摘要：

An earlier gravity flow theory (Colbeck 1971) treated snow as a homogeneous and uniform medium. The theory is expanded here to include the effects of ice layers and flow channels. Two examples are constructed and compared with observed runoff. In this particular situation, the results suggest that most of the water moves down flow channels. © 1979.

引用

页码：37 / 45

页数：9

共 19 条

[1]

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[2]

Colbeck, Effects of stratigraphic layers on water flow through snow, Research Report 311, (1973)

[3]

Colbeck, A theory for water flow through a layered snowpack, Water Resour. Res., 11, 2, pp. 261-266, (1975)

[4]

Colbeck, Short-term forecasting of water run-off from snow and ice, J. Glaciol., 19, 81, pp. 571-588, (1977)

[5]

Colbeck, Physical principles of water flow through snow, Advances in Hydroscience, 11, pp. 165-206, (1978)

[6]

Corps of Engineers, Snow Hydrology, (1956)

[7]

Dunne, Price, Colbeck, The generation of runoff from subarctic snowpacks, Water Resour. Res., 12, 4, pp. 677-685, (1976)

[8]

Freeze, A stochastic-conceptual analysis of one-dimensional groundwater flow in nonuniform homogeneous media, Water Resour. Res., 11, 4, pp. 725-741, (1975)

[9]

Gerdel, The dynamics of liquid water in deep snow-packs, Transactions, American Geophysical Union, 26, 1, pp. 83-90, (1945)

[10]

Gerdel, The transmission of water through snow, Transactions, American Geophysical Union, 35, 3, pp. 475-485, (1954)

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