摘要:From a methodological point of view, hydrological modelling
appears to offer a great potential for spatial analysis. However
among classes of models, only physical models consider the
spatial dimension as a variable. The topography and the land
cover are the two major spatial components involved in that
type of models. The production of a relevant DTM requires the
use of iterative interpolation procedures. Land cover and its
changes can be monitored and entered into modelling from
remote sensing images through a normalized Vegetation index. The GIS approach can be integrated at different levels
within hydrological modelling, with object oriented GIS seen
as the highest level.