Fig. 6. Simulated water content at 60 cm using K_s and L = 0.5 and by setting the water table at the 3-m depth, without readjusting the soil-dependent transpiration parameters (filled squares), after readjustment (open diamonds). For comparison purpose, results calculated by neglecting the influence of the water table are given (cross). Mean and spread of the measured soil moisture content are shown (thick line: mean; thin lines: mean ± sd).