WMS:TR-20 Kinematic Wave: Difference between revisions
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:<math>Q = xA^m </math> | :<math>Q = xA^m </math> | ||
where <math>Q</math> is the discharge, <math>A</math> is the valley storage area divided by length and <math>x</math> and <math>m</math> are the coefficient and exponent of the relationship describing the reach and maximum inflow hydrograph peak discharge. | where <math>Q</math> is the discharge, <math>A</math> is the valley storage area divided by length and <math>x</math> and <math>m</math> are the coefficient and exponent of the relationship describing the reach and maximum inflow hydrograph peak discharge. | ||
Latest revision as of 22:03, 22 February 2013
The kinematic wave method uses two different rating coefficients, x and m, in the following equation:
where is the discharge, is the valley storage area divided by length and and are the coefficient and exponent of the relationship describing the reach and maximum inflow hydrograph peak discharge.
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