TUFLOW 2D Cell Size Selection: Difference between revisions
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This test is designed to simulate flood wave propagation down a river valley following the failure of a dam. The valley DEM is ~0.8 km by ~17 km and the valley slopes downstream on a slope of ~0.01 in its upper region, easing to ~0.001 at lower elevations. <br> |
This test is designed to simulate flood wave propagation down a river valley following the failure of a dam. The valley DEM is ~0.8 km by ~17 km and the valley slopes downstream on a slope of ~0.01 in its upper region, easing to ~0.001 at lower elevations. <br> |
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[[File:Mesh_Converge_Model_Description_001.png|400px]]<br> |
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[[File:Mesh_Converge_Model_Elevation_001.png|500px]]<br> |
[[File:Mesh_Converge_Model_Elevation_001.png|500px]]<br> |
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The inflow hydrograph shown below is applied as a boundary condition at the upstream end of the valley. <br> |
The inflow hydrograph shown below is applied as a boundary condition at the upstream end of the valley. <br> |
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Revision as of 12:40, 24 May 2018
This page is currently under construction.
Cell size convergence is an important concept in flood modelling.
This test is designed to simulate flood wave propagation down a river valley following the failure of a dam. The valley DEM is ~0.8 km by ~17 km and the valley slopes downstream on a slope of ~0.01 in its upper region, easing to ~0.001 at lower elevations.
The inflow hydrograph shown below is applied as a boundary condition at the upstream end of the valley.
Rural Catchment Assessment Results =
