A Mesoscale Analysis of the Impact of Snowpack on Climate Variability
in the Sierra Nevada Region
Jiming Jin and Norman L. Miller
Contact: Jiming Jin, 510/486-7551, JimingJin@lbl.gov
Research Objective
Greater than 70% of the annual streamflow in the western United
States is derived from snowpack (Cayan, 1996). Hence, accurately
forecasting snowpack is essential to this region's economy and well-being,
and numerical models are necessary (and powerful) tools for this
purpose. The objectives of this study were to evaluate the snow
scheme with an advanced mesoscale model, using observational evidence,
and to investigate the impact of snowpack on climate variability
in the Sierra Nevada region.
To continue reading more about this project, view the
1-page pdf here.
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Comparison of simulations and observations averaged over the Sierra Nevada region for the period of April 2-June 30, 1998: (a) Snow water equivalent (mm); (b) 2 m height air temperature (degrees C); (c) Precipitation (mm). Obs is observations, Simu is the 12 km resolution simulation with no SWE assimilation, and SimuAs is the 12 km resolution simulation with SWE assimilation.
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