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Snow Water Equivalent (SWE) is a common snowpack measurement. It is defined as the amount of water contained within the snowpack. These snowpack projections are produced by using a land surface/hydrology model known as the Variable Infiltration Capacity (VIC) model. The VIC model uses high resolution LOCA precipitation and temperature data from Scripps Institution Of Oceanography as input to calculate SWE and a suite of additional parameters. Details are described in Pierce et al., 2016 and Pierce et al., 2014.