WORLD METEOROLOGICAL ORGANIZATION |
HOMS COMPONENT |
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Explanation of the criteria for classification and numbering of components | K35.1.05 (JUN 00) |
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Explanation of the dates on the component's description | ||
NUMERICAL SOLUTION OF THE NON-LINEAR MUSKINGUM METHOD |
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1. Purpose and objectives Flood routing by the Muskingum method. This component takes into account the change of velocity due to discharge, and the method is reformulated as a non-linear problem which is solved using a computer program. 2. Description The inflow hydrograph is known and the outflow discharge is to be obtained. Four parameters are introduced to define how the values of
Muskingum's K and x are related to discharge. All these parameters can be
determined from the hydraulic properties of the channel. 3. Input Inflow and outflow hydrographs of the channel. 4. Output 5. Operational requirements and restrictions The user should be familiar with the basic theory of the method. 6. Form of presentation Manual in English, printed listing of program and floppy diskette. 7. Operational experience It has been applied successfully in different river reaches in China. 8. Originator and technical support Zhao Ren-jun and Wang Pei-len, Hohai University, Nanjing, China 9. Availability From the HOMS National Reference Centre for China. 10. Conditions on use Cost of reproduction and mailing.
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(First entered:15 APR 88 | Last updated: 7 APRIL 2000) |