WMS:Rational Method: Difference between revisions

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All of the computations for peak flows, hydrographs, and routing are done within WMS.
All of the computations for peak flows, hydrographs, and routing are done within WMS.
The Rational Method interface is included will all [http://www.aquaveo.com/software/wms-pricing paid editions] of WMS. [[Category:Link to Store]]


==Saving and Running a Rational Method Simulation==
==Saving and Running a Rational Method Simulation==

Revision as of 16:56, 7 January 2016

WMS includes an interface to the rational method which can be used for computing peak flows on small urban and rural watersheds. The interface includes the capability to combine runoff from multiple basins. Two different methods for determining peak flows/hydrographs at downstream confluences are available.

Traditionally a time of concentration is determined at a downstream confluence by determining the longest combination of time of concentration and routing travel time. Given a time of concentration for the outlet, a rainfall intensity can be determined from a rainfall-intensity-duration curve and a peak flow computed. The hydrograph for the confluence is then determined in the same manner they are determined for sub-basins; by using the peak flow, time of concentration, and a dimensionless hydrograph.

Alternatively, hydrographs for the sub-basins can be computed and then routed (lagged) and combined by summing at the confluence points. When using this method detention basins may be defined at confluence points in order to determine the effect of storage on the computations.

All of the computations for peak flows, hydrographs, and routing are done within WMS.


The Rational Method interface is included will all paid editions of WMS.

Saving and Running a Rational Method Simulation

The Save Simulation command in the Rational menu can be used to save the topologic tree structure with any rational method parameters which have been defined. The Read Simulation command will restore the tree and parameters so that the user may continue with a particular model.

Important Limitations

Due to assumptions regarding homogeneity of rainfall and equilibrium conditions at the time of peak flow, the rational method should not be used on areas larger than about 1 square mile without subdividing the overall watershed into sub-basins including the effect of routing through any drainage channels.

WMS includes two different methods for determining runoff from larger watersheds, subdivided into smaller sub-basins, including the ability to account for routing and lag through drainage channels and detention basins.

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