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This paper presents further snow module calibration work.
Additional calibration of the snow module was done for California using snow course data in the Sierra Nevada and Trinity Mountains, MODIS snow cover data, and mapped glaciers.
The calibration of snow module parameters was done to optimize the discharge estimated by the CA-BCM in comparison to reconstructed unimpaired flows for 21 mountain basins draining to the San Francisco Bay Delta (Figure 1).
Using PET and gridded precipitation, maximum and minimum air temperature, and the approach of the National Weather Service Snow-17 model (Anderson 1976), the snow module accumulates, sublimates, and melts snow to produce available water (Figure 2).
To ensure correct timing of snow accumulation and melt on a volume basis, calibration of the snow module was done to compare average monthly flows from the CA-BCM to unimpaired flows to the Central Valley for 21 basins that were based on reconstructions (see DWR 2007 for methodology).
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We characterize the results for a 30-year period from 1981 2010, and changes from 1951 1980, and assess model performance for the runoff and snow modules by using streamgages and snow courses.
Some of these factors are debris, water and/or snow, temperature, module mismatching and/or PV module aging [19].
Ice-water content variations in winter are reasonably simulated by the new module for different snow cover scenarios.
Not only does it include a GPS module to help you get back to that snow bunny, it also has an integrated display on the sleeve and audible instructions that are pumped through the hood.
The warning system has also an additional module that accounts for the effects of snowmelt and snow accumulation (Martelloni et al. 2013).
The BCM has several subroutines or modules: the calculation of potential and actual evapotranspiration and climatic water deficit; snow accumulation and melt; available water; and recharge and runoff (Figure 2).
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