Precipitation Downscaling on the West Coast of Norway: Comparison with Observational Network
نویسندگان
چکیده
High frequency observations from a field campaign have been compared with time-step precipitation in the WRF regional climate model. Two microphysical schemes of different levels of sophistication have been tested. Both of the schemes generally reproduce the observed precipitation, yet the produced level of wetness is somewhat high, and the intensities rather low. Typical simulated intensities are about 9mm/hr, as opposed to the observed values of approximately 15mm/hr. The simpler scheme performs better in complex terrain. Both schemes show limited skill on flat land.
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