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    Extreme-Value Statistics for Snowpack Water Equivalent in the Northeastern United States Using the Cooperative Observer Network 

    Source: Journal of Applied Meteorology:;1996:;volume( 035 ):;issue: 005:;page 706
    Author(s): Wilks, Daniel S.; McKay, Megan
    Publisher: American Meteorological Society
    Abstract: A procedure is developed to estimate extreme-value statistics for snowpack water equivalent (SWE) using historical snow depth measurements at cooperative observer stations in the northeastern United States. The method ...
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    A Physically Based Model of Soil Freezing in Humid Climates Using Air Temperature and Snow Cover Data 

    Source: Journal of Applied Meteorology:;1996:;volume( 035 ):;issue: 006:;page 1009
    Author(s): DeGaetano, Arthur T.; Wilks, Daniel S.; McKay, Megan
    Publisher: American Meteorological Society
    Abstract: A one-dimensional heat flow model is developed to estimate depths of soil freezing and thawing using a daily time step. This physically based model assumes near-saturated soil moisture conditions and simulates freezing ...
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    Automated Quality Control Procedure for the "Water Equivalent of Snow on the Ground" Measurement 

    Source: Journal of Applied Meteorology:;1995:;volume( 034 ):;issue: 001:;page 143
    Author(s): Schmidlin, Thomas W.; Wilks, Daniel S.; McKay, Megan; Cember, Richard P.
    Publisher: American Meteorological Society
    Abstract: Snow water equivalent (SWE) has been measured daily by the United States National Weather Service since 1952, whenever snow depth is 2 in. (5 cm) or greater. These data are used to develop design snow loads for buildings, ...
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