A semi-distributed watershed model was developed that conceptualizes the ca
tchment as a cascade of nonlinear storage elements whose geometric dimensio
ns are derived from the Horton-Strahler ordering of the stream network. Eac
h storage element represents quick storm runoff over land or in a channel s
egment. The physically based groundwater submodel is parameterized through
the application of the Brutsaert-Nieber recession flow analysis and it prov
ides continuous baseflow separation. The model requires the calibration of
seven parameters from a one year rainfall-runoff record. It was tested on t
he Mahantango Creek watershed in the Susquehanna River basin, Pennsylvania.
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