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Runoff occurs when precipitation exceeds the infiltration capacity of soils. There are several mechanisms of runoff generation including Horton overland flow, subsurface stormflow, and saturation overland flow. The characteristics of runoff from a watershed include the peak discharge, hydrograph shape, total runoff volume, and frequency of peak flows. These characteristics are influenced by watershed properties such as drainage area, slope, roughness, storage, drainage density, channel length, and anteceden

Author

rienalen placa

Language

EN