Geoscience Reference
In-Depth Information
Insolation
Precipitation
Temperature
Snow
Rain
Snow Pack
Melt
Runoff
Supply
Upstream
Evapotranspiration
Surface
Runoff
Upper Soil
Moisture
Downstream
Upstream
Percolation
Evapotranspiration
Lower Soil
Moisture
Interflow
Downstream
Upstream
Deep Percolation
Evapotranspiration
Ground
water
Groundwater
Moisture
Downstream
Upstream
Evaporation
Surface
Moisture
Downstream
Fig. 6.2 Scheme of the model
governed by continuity equations with linear loss/transformation coefficients
(mathematical equations are not shown here due to space limits; for details, see
Croley and He
2005
,
2006
).
The DLBRM hydrology component requires 16 input variables for each of
the cells (Tables
6.1
and
6.2
). The model output includes: for every cell in the
watershed grid, basin outflow, surface runoff, evapotranspiration, infiltration,
