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FLOOD10338
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Last modified
1/26/2010 10:13:04 AM
Creation date
10/19/2007 1:03:36 PM
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Floodplain Documents
County
Statewide
Basin
Statewide
Title
TR-20 Computer Program for Project Formulation Hydrology
Date
5/1/1983
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />3-9 <br /> <br />~ <br /> <br />The holdout hydrograph at a flood control structure site is a discharge <br />hydro graph consisting of the difference between the inflow and outflow <br />hydrographs. The discharge values will be negative when the outflow <br />exceeds the inflow. At present, the holdout hydrographs can be obtained <br />only at the structure sites. This version of TR-20 will not allow the <br />negative portion of the holdout hydrograph to be reach routed downstream. <br />Furthermore, the routing coefficient in the Modified Att-Kin reach <br />routing method varies with the magnitude of the inflow hydrograph peak <br />and volume (See theory in Appendices G and H). Thus, the holdout <br />portion of a storm hydrograph cannot be routed downstream separately <br />with any degree of consistency to compare with the unmodified total <br />storm hydrograph. The amount of attenuation and kinematic translation <br />will vary with magnitude of the hydro graph being routed. Additional <br />study will determine what shortcuts or improvements may be needed to <br />continue use of this routing technique commonly called tabular routing. <br />The holdout procedure must be completed by other means at this time. <br /> <br />~. <br /> <br />The holdout procedureVis to route the holdout hydrographs from structure <br />sites for a particular storm downstream without adding any uncontrolled <br />area. This entails a separate set of Standard Control statements that <br />develop the inflow hydrographs above the structures, reservoir routes <br />through the structures, then reach routes through consecutive reaches <br />generating output files for evaluation at selected points of interest. <br />The holdout hydrographs from the structures must be combined algebraically <br />with the proper timing at all stream junctions to form a composite <br />holdout hydrograph. The modified storm hydrograph at any point of <br />interest may be obtained by subtracting the composite holdout hydrograph <br />from the total storm hydrograph obtained by the regular TR-20 procedure. <br />The advantage of the procedure is that individual site or group of <br />site holdout hydrographs can be developed and routed downstream and <br />subtracted from the composite holdout hydrograph to analyze their <br />separate effect. <br /> <br />. <br /> <br />To properly evaluate the downstream effect of the combined structure <br />release rates and their timing, the main time increment should be <br />small enough to adequately define the hydrograph peak yet large enough <br />so that the entire hydrograph will fit within the 300 elements of the <br />hydrograph.. <br />
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