WMS:Putnam Lag Time Equation: Difference between revisions
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where: | where: | ||
<math>T_{LAG}</math> = lag time in hours. | |||
L = maximum flow length in miles. | <math>L</math> = maximum flow length in miles. | ||
S = weighted slope along the maximum flow path in ft/mile. | <math>S</math> = weighted slope along the maximum flow path in ft/mile. | ||
<math>I_a</math> = Impervious cover as a fraction. | |||
This equation was used for watersheds ranging in size from 0.3 to 150 sq. miles, impervious covers less than 0.3 and a ratio of between 1.0 and 9.0. | This equation was used for watersheds ranging in size from 0.3 to 150 sq. miles, impervious covers less than 0.3 and a ratio of between 1.0 and 9.0. |
Revision as of 20:50, 26 February 2013
Putnam (1972) developed a lag equation for watersheds around the Wichita, Kansas area as follows:
where:
= lag time in hours.
= maximum flow length in miles.
= weighted slope along the maximum flow path in ft/mile.
= Impervious cover as a fraction.
This equation was used for watersheds ranging in size from 0.3 to 150 sq. miles, impervious covers less than 0.3 and a ratio of between 1.0 and 9.0.
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