!output flux and state variable @@ -98,15 +100,15 @@ subroutine wrf_cpl_HYDRO(HYDRO_dt,grid,its,ite,jts,jte) if(.not. RT_DOMAIN(did)%initialized) then call MPP_LAND_INIT() !yw nlst_rt(did)%nsoil = config_flags%num_soil_layers !nlst_rt(did)%nsoil = model_config_rec%num_me...
Among all the variables that relate to the water cycle, precipitation is considered the most important variable for streamflow modeling and forecasting. Uncertainty in the precipitation measurement is one of the chief limitations in the hydrological modeling where the hydrology model is run in a stand...
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A new wrfinput_d0x.nc file is required due to some variable changes and can be generated using the create_Wrfinput.R script. Note: the v3.0 shell script for creating the wrfinput_d0x.nc file from the geogrid file will not work for v5; use the v5 script provided on the WRF-Hydro ...
Location MSGC01 (Outlet) Variable Sediment concentration Sediment flux Correlation Coefficient 0.57 0.62 RMSE 19,692.64 mg/L 65,321.10 t/d NSE 0.25 0.28 KGE 0.44 0.30 We notice that the model simulated only one peak for sediment flux and sediment concentration, while the observation exhibited ...
Snow influences land–atmosphere interactions in snow-dominated areas, and snow melt contributes to basin streamflows. However, estimating snowpack properties such as the snow depth (SD) and snow water equivalent (SWE) from land surface model simulations