1 edition of Snowmelt-frozen soil characteristics for a subarctic setting found in the catalog.
Snowmelt-frozen soil characteristics for a subarctic setting
by Institute of Water Resources, University of Alaska in Fairbanks, AK
Written in English
|Statement||Douglas L. Kane ... [et al.].|
|Series||Report (University of Alaska, Fairbanks. Institute of Water Resources) -- IWR-84|
|Contributions||Kane, Douglas L., University of Alaska, Fairbanks. Institute of Water Resources.|
|The Physical Object|
|Pagination||vi, 64 p. :|
|Number of Pages||64|
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Open Library is an open, editable library catalog, building towards a web page for every book ever published. Publisher: Institute of Water Resources, University of Alaska |. Snowmelt and Frozen Soil [Based on class notes by Erin Brooks and the text by Dingman ()] I. Snow Hydrology Terms Precipitation: the depth of rainfall plus the water equivalent of snow, sleet, and hail falling during a given storm or measurement period Snowfall: the incremental depth of snow and other forms of solid precipitation.
In China, seasonally frozen soil covers slightly more than half (%) of the total land area (Zhou et al. The amount of snowmelt infiltration, which.
through relations between soil physical and soil hydraulic properties that establish the magnitudes and ranges of properties in the boreal forest biome in interior Alaska.
/WR Snowmelt and Frozen Soil I. Snow Hydrology Terms Precipitation: the depth of rainfall plus the water equivalent of snow, sleet, and hail falling during a given storm or measurement period.
Snowfall: the incremental depth of snow and other forms of solid precipitation accumulating on the surface during a given storm or measurement period.
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