| BASEMENTBasic Simulation Environment for computation of environmental flow and natural hazard simulationLaboratory of Hydraulics, Hydrology and Glaciology (VAW)ETH Zurich | ![]() |
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Hi Everyone
I'm having problems with my model using BASEHPC:
I'm facing the problem, that when modelling bridges and large culverts with h-Q relations (linked boundaries) i have big differences in the upstream and downstream water depth. This is to be expected with "no_momentum" but i also tried the other types.
While this wouldn't be as big of a problem for one linked boundary, in my model domain i have multiple in short succession occurring bridges/culverts, resulting in a really strange longitudinal water surface elevation profile along the river.
Regarding mesh quality: i have a really high resolution DEM, i implemented max_area of my cells at and around the boundary at 0.1 or 0.2. So this shouldn't be the problem.
For h-Q i used normal depth flow calculations, which are obviously quite sensitive to chosen slope and roughness value....
Is there a "BEST" approach to minimize or even eliminate these jumps in water depth/water surface elevation?
And what is the best way to implement h-Q relations when using BASEHPC? Like sort of a checklist on important things when creating the h-Q relations.
*EDIT:
In BASEMD there's the Gate boundary, why is this not implemented in BASEHPC?
Last edited by wasserbändiger (2026-08-03 07:45:28)
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