the following five parameters
were adjusted: (1) Storage coefficient of direct runoff
kd; (2) storage coefficient of
interflow ki; (3) drainage density d; (4) the fraction of surface runoff from snowmelt; and
(5) the recession constant krec for the decreasing saturated hydraulic conductivity with
increasing depth. For the groundwater flow, adjusted parameters (6–7) are the hydraulic
conductivity in the X
/media/ces/2010_016.pdf