|Owners:||Edward Morgan · Jeff Sadler|
|Resource type:||Model Program Resource|
|Created:||Jan 19, 2017 at 4:33 a.m.|
|Last updated:||May 14, 2017 at 3:36 a.m. by Edward Morgan|
This process component is part of a spatially-distributed hydrologic model called TopoFlow, but it can now be used as a stand-alone model. It uses the "diffusive wave" method to compute flow velocities for all of the channels in a D8-based river network. This method includes a pressure gradient term that is induced by a water-depth gradient in the downstream direction. This means that instead of using bed slope in Manning's equation or the law of the wall, the water-surface slope is used.
How to cite
This resource is shared under the Creative Commons Attribution CC BY.http://creativecommons.org/licenses/by/4.0/
|Peckham, Scott||CSDMS, INSTAAR, University of Colorado||1560 30th St., Boulder, CO, USA, 80303||3034926752|
|Operating System||Unix, Linux, Mac OS, Windows|
|Software Repository||http:// https://github.com/peckhams/topoflow|
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