Calculation of Hydrologic Parameters Using CRWR-PrePro
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Calculation of Hydrologic Parameters Using CRWR-PrePro. Francisco Olivera, PhD Center for Research in Water Resources University of Texas at Austin. Hydrologic Parameters. Watershed Abstractions and routing method Parameters Stream Routing method Parameters.
Calculation of Hydrologic Parameters Using CRWR-PrePro
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Calculation of Hydrologic ParametersUsing CRWR-PrePro Francisco Olivera, PhD Center for Research in Water Resources University of Texas at Austin
Hydrologic Parameters • Watershed • Abstractions and routing method • Parameters • Stream • Routing method • Parameters
Watershed Abstractionsand Routing Method • Abstractions: precipitation/excess precipitation transformation • SCS curve number method • Initial loss + constant rate loss • Routing: excess precipitation/runoff flow transformation • Soil Conservation Service (SCS) synthetic unit hydrograph
Watershed Abstractions Precipitation (mm) Excess precipitation (mm) Soil properties Excess precipitation = f(Precipitation, Soil properties)
Watershed Routing Excess precipitation (mm/hr) Watershed Runoff flow (m3/s)
Watershed Routing Excess precipitation (mm/hr) Excess precipitation and Runoff flow Runoff flow (m3/s) Time Runoff flow = f(Excess precipitation, Watershed hydrologic properties)
Hydrologic Parameters • Watershed • Abstractions and routing method • Parameters • Stream • Routing method • Parameters
Watershed Parameters • Area • Average curve number • Initial + constant rate loss • Length of longest flow-path • Slope of longest flow path • Lag time
Watershed Lag-Time (SCS) tp: lag-time (min) LW: length of longest flow-path (ft) S: slope of the longest flow-path (%) CN: average Curve Number Dt: analysis time step
Watershed Lag-Time (L/V) tp: watershed lag-time (min) Lw: length of longest flow-path (ft) Vw: longest flow-path average velocity (m/s) Dt: analysis time step
Hydrologic Parameters • Watershed • Abstractions and routing method • Parameters • Stream • Routing method • Parameters
Pure-Lag Method • Flow is delayed a fixed amount of time tlag. tlag: flow time in the reach I: inflow to the reach Q: outflow from the reach
Muskingum Method • Flow is delayed a fixed amount of time K, and redistributed around its centroid. S: storage in the reach K: flow time in the reach (Dt < K < Dt/2X) X: storage parameter I: inflow to the reach Q: outflow from the reach Dt: analysis time step
Routing Method Flow time (Ls/Vs) Ls/Vs < Dt Ls/Vs > Dt Pure LagRouting MuskingumRouting Ls: length of the stream Vs: flow velocity in the stream Dt: analysis time step
Hydrologic Parameters • Watershed • Abstractions and routing method • Parameters • Stream • Routing method • Parameters
Pure Lag Parameters tlag: flow time in the reach (min) Ls: reach length (m) Vs: reach average velocity (m/s)
Muskingum Parameters K: flow time in the reach (hr) [Muskingum K] X: storage parameter [Muskingum X] Ls: reach length (m) Vs: reach average velocity (m/s) n: number of sub-reaches Dt: analysis time step