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Introduction to Hydrologic Science
The Conservation Equations
The Watershed Drainage Basin
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annual approach aquifer areal atmosphere average calculated Chapter climate compute concentration curve Darcy's law decrease density depth determined developed discharge discussed distribution drainage basin effects elevation energy Equa Equation estimate evaporation evapotranspiration event Example flood flux forest function gage given global gradient ground water ground-water flow heat hydraulic conductivity hydrograph hydrologic cycle increase infiltrometer inflow intercepted water isohyetal lake latent heat layer measured melt method occurs outflow overland flow precipitation quantity radiation rain rainfall recharge region relation relative response Richards equation River runoff sample saturated saturated zone seasonal shown in Figure shows slope snow snowmelt snowpack soil solar spatial storage storm stream streamflow subregion surface temperature tion typically U.S. Geological Survey unit unsaturated usually values variability velocity vertical volume water content water equivalent water input water table water vapor water-balance watershed weight wind speed zone