Keith Cherkauer
May 18, 1996
This subroutine computes surface runoff, infiltration into the soil, and through the soil layers, and out the bottom as baseflow. Runoff is controlled by the Arno curve, which assumes that moisture in the top layer is not evenly distributed.
Liang, X., D. P. Lettenmaier, E. F. Wood, and S. J. Burges, A Simple hydrologically Based Model of Land Surface Water and Energy Fluxes for GSMs, J. Geophys. Res., 99(D7), 14,415-14,428, 1994.
Variable |
Type |
Units |
Description |
|
layer |
layer_data_struct * |
N/A |
Structure contains soil layer variables
|
|
soil_con |
soil_con_struct |
N/A |
Structure contains soil parameters
|
|
mu |
double |
fraction |
Fraction of grid cell that receives precipitation |
|
x |
double |
fraction |
Fraction of mu that receives precipitation that exceeds the interception capacity of the vegetation |
|
ppt |
double |
mm |
Total precipitation |
|
dt |
int |
hr |
Model time step |
|
Tlayer |
int |
N/A |
Total number of thermal solution nodes |
Variable |
Type |
Units |
Description |
|
runoff |
double * |
mm |
Runoff from grid cell |
|
baseflow |
double * |
mm |
Baseflow from grid cell |
|
energy |
energy_bal_struct * |
N/A |
Structure contains energy balance variables
|
|
layer |
layer_data_struct * |
N/A |
Structure contains soil layer variables
|
Page Last Modified on 2/9/98