Derives and validates the hyperbolic HSWEMED model coupling shallow water moments, suspended load, variable density, and bedload morphodynamics with erosion-deposition, showing improved accuracy on dam-break tests.
A depth-averaged non-cohesive sediment transport model with improved discretization of flux and source terms
2 Pith papers cite this work. Polarity classification is still indexing.
2
Pith papers citing it
representative citing papers
SWEMED1 has a weakly hyperbolic fully-settled water-at-rest equilibrium without indicated instability; fast-limit scaling produces a suspended equilibrium still weakly hyperbolic due to transport closure.
citing papers explorer
No citing papers match the current filters.