📄 topmodel_grass_param.txt
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# Catchment nameSubcatchment 1# A: Total catchment area# [m^2]## qs0: Initial subsurface flow per unit area# [m/h]# "The first streamflow input is assumed to represent# only the subsurface flow contribution in the watershed."# - Ref[S.C.Liaw]# lnTe: Areal average of ln(T0) = ln(Te)# [ln(m^2/h)]# m: Model parameter# [m]# Sr0: Initial root zone storage deficit# [m]# Srmax: Maximum root zone storage deficit# [m]# td: Unsaturated zone time delay per unit storage deficit# ( > 0.0) [h]# OR# -alpha: Effective vertical hydraulic gradient# ( <= 0.0) -10 means that alpha = 10# vch: Main channel routing velocity# [m/h]# vr: Internal subcatchment routing velocity# [m/h]## infex: Calculate infiltration excess if not zero (integer)# K0: Surface hydraulic conductivity# [m/h]# psi: Wetting front suction# [m]# dtheta: Water content change across the wetting front## nch: Number of distance increments## d: Distance from catchment# [m]# The first value should be the mainstream distance from# the subcatchment outlet to the catchment outlet.# Ad_r: Cumulative area ratio of subcatchment (0.0 to 1.0)# The first value should be zero.# # A# [m^2] 1# qs0 lnTe m Sr0 Srmax td/alpha vch vr 3.28e-05 5. 0.032 0.002 0.05 50. 3600. 3600. # infex K psi dtheta 1 1. 0.02 0.1 # nch 3# d Ad_r 500 0 1000 0.5 1500 1
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