A new Geomorphologic Instantaneous Unit Hydrograph is proposed, It includes
the position of the tributary links in the fluvial network which was not c
onsidered in previous developments, The resulting hydrograph shows signific
ative differences with the original model of Rodriguez-Iturbe and Valdes (1
979), modifying the ordinate and the time of ocurrence of the peak. These d
ifferences increase when the overland flow effects are included. There is n
ot a unique hydrograph for distinct watersheds with similar Horton ratios.
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