Influence of Subgrid Variability on Soil Moisture and Latent Heat Flux

نویسندگان

  • S. J. Ghan
  • J. C. Liljegren
  • J. C. Doran
چکیده

Soil hydrology is highly nonlinear. As surface soil becomes To characterize the subgrid variability in surface hydrology at saturated with water, excess water runs off in streams. If the the SGP site, we drive a land surface model (the parameters that influence surface soil water vary widely within Biosphere-Atmosphere Transfer Scheme [BATS]; Dickinson a general circulation model (GCM) grid cell, the grid cell et al. 1993) with meteorology, radiation, soil characteristics, mean soil moisture and latent heat flux could be very sensitive and vegetation characteristics observed at 111 Oklahoma to the treatment of subgrid variability. MESONET stations for the period from June to August 1995.

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تاریخ انتشار 1997