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.
Bedload transport in shallow water models: Why splitting (may) fail, how hyperbolicity (can) help
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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.
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