WMS:Riverside County Lag Time Equation: Difference between revisions

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where:
where:


T<sub>LAG</sub> - lag time in hours.
T<sub>LAG</sub> = lag time in hours.


L - maximum flow length in miles.
L = maximum flow length in miles.


L<sub>ca</sub> - length to the centroid in miles.
L<sub>ca</sub> = length to the centroid in miles.


S - weighted slope along the maximum flow path length in ft/mile.
S = weighted slope along the maximum flow path length in ft/mile.


The typical characteristics of watersheds for which the Riverside County equations were used include the following:
The typical characteristics of watersheds for which the Riverside County equations were used include the following:

Revision as of 20:55, 26 February 2013

The Riverside County Flood Control and Water Conservancy District developed three different lag equations corresponding to mountainous, foothill, and valley areas near Riverside County, California (Anonymous, 1963).

File:Image113.gif
(Mountainous) 15.19
File:Image114.gif
(Foothills) 15.20
File:Image115.gif
(Valleys) 15.21

where:

TLAG = lag time in hours.

L = maximum flow length in miles.

Lca = length to the centroid in miles.

S = weighted slope along the maximum flow path length in ft/mile.

The typical characteristics of watersheds for which the Riverside County equations were used include the following:

Areas from 2 to 650 square miles.


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