Chezy equation: Difference between revisions
From Glossary of Meteorology
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Revision as of 17:39, 26 January 2012
Chezy equation
An empirical equation relating the mean velocity of flow to channel characteristics.
It is expressed as where C is the Chezy resistance coefficient, Sf the gradient of the total head line, and R the hydraulic radius. For discharge Q, where A is the cross-sectional area.
See Manning equation.
See Manning equation.