A distributed hydrological model, water and energy transfer processes (WEP)
model, is developed to simulate spatially variable water and energy proces
ses in watersheds with complex land covers. In the model, state variables i
nclude depression storage on land surfaces and canopies, soil moisture cont
ent, land surface temperature, groundwater tables and water stages in river
s, etc. The subgrid heterogeneity of land use is also taken into considerat
ion by using the mosaic method. For hydrological processes, evapotranspirat
ion is computed by the Pemnan-Monteith equation, infiltration excess during
heavy rains is simulated by a generalized Green-Ampt model, whereas satura
tion excess during the remaining periods is obtained by doing balance analy
sis in unsaturated soil layers. A two-dimensional simulation of multilayere
d aquifers is performed for groundwater flow. Flow routing is conducted by
using the kinematic wave method in a one-dimensional scheme. For energy pro
cesses, short-wave radiation is based on observation or deduced from sunshi
ne duration, long-wave radiation is calculated according to temperatures, l
atent and sensible fluxes are computed by the aerodynamic method and surfac
e temperature is solved by the force-restore method. In addition, anthropog
enic components, e.g. water supply, groundwater lift, sewerage drainage and
energy consumption, etc. are also taken into account. The model is applied
to the Ebi River watershed (27 km(2)) with a grid size of 50 m and a time
step of 1 h. The model is verified through comparisons of simulated river d
ischarges, groundwater levels and land surface temperatures with the observ
ed values. A comparison between water balance at present (1993) and that in
the future (2035) is also conducted. It is found that the hydrological cyc
le in the future can be improved through the implementation of infiltration
trenches for the storm water from urban canopies. Copyright (C) 2001 John
Wiley & Sons, Ltd.