Constant K in Hydrologic Channel Routing Formulas

Constant K is for the catchment to be determined by flood hydrograph characteristics of the catchment. And is denoted by K.

Hydrologic Channel Routing formulas that make use of Constant K

fxTotal Wedge Storage in Channel ReachGo

fxEquation for Linear Storage or Linear ReservoirGo

fxOutflow given Linear StorageGo

fxStorage in Beginning of Time IntervalGo

fxStorage during end of time interval in Muskingum method of RoutingGo

fxMuskingum EquationGo

fxChange in Storage in Muskingum Method of RoutingGo

What is the Constant K?

Constant K is for the catchment to be determined by flood hydrograph characteristics of the catchment.

Can the Constant K be negative?

{YesorNo}, the Constant K, measured in {OutputVariableMeasurementName} {CanorCannot} be negative.

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