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This paper tried to clarify the effects of capillary rise on subsurface runoff through a recently suggested water balance model for representative elementary watersheds (REWs). We focused on saturated zone water balance of a REW model effected by the capillary rise, in comparison with to the Tank model. The results and discussions on the comparison led the followings: (1) Capillary rise is effective under arid climate than humid climate. (2) This tendency is enhanced under climates with clear difference between wet and dry seasons. (3) REW models have potential to describe and diagnose basin's processes based on the mass and momentum balance equations better than Tank models and other lumped water balance models. (4) REW models can be more suitable than Richards equation based models under arid climate if user's requirement for model structure is only unsaturated and saturated zones.

EFFECT OF CAPILLARY RISE ON SUBSURFACE RUNOFF IN THE REW MODELING FRAMEWORK