Model:TopoFlow-Channels-Diffusive Wave: Difference between revisions
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|Extended model description=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. | |Extended model description=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. | ||
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{{Model keywords | {{Model keywords | ||
|Model keywords=basins | |Model keywords=basins | ||
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{{Model technical information | {{Model technical information | ||
|Supported platforms=Unix, Linux, Mac OS, Windows | |Supported platforms=Unix, Linux, Mac OS, Windows | ||
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|CMT component=Yes | |CMT component=Yes | ||
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{{CSDMS coupled models | {{CSDMS coupled models | ||
|Animation model name=TopoFlow | |Animation model name=TopoFlow | ||
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|Animation model name=TopoFlow-Diversions | |Animation model name=TopoFlow-Diversions | ||
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