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Quantitative Geomorphology of Drainage Basins and Channel
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amount analysis annual applied aquifer average basin capacity cause cent channel characteristics coefficient computed concentration considered correlation curve density depends depth determined developed discharge distribution drainage effect Engineers equal equation estimated evaporation example factors flood flow frequency function gage given glacier groundwater heat hydraulic hydrograph hydrologic important increase indicate infiltration length less limited load loss mass material maximum mean measured method moisture natural normal observed obtained occur period plotted precipitation pressure probability rainfall range ratio records reference regions relation relatively represents reservoir result River runoff sample sediment shown shows slope snow soil storage storm stream studies supply surface Table temperature tion United usually values variables variation various watershed Weather weight wind