A discontinuous Galerkin method with a bound preserving limiter for the advection of non-diffusive fields in solid Earth geodynamics
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文摘
Discontinuous Galerkin method for advection of compositional fields in mantle convection. Bound preserving limiter is used to maintain sharp boundaries (<0.02% overshoot). Falling box benchmark is used to demonstrate the method. Results are compared to a finite element method using entropy-viscosity stabilization. Can be used in 2-D and 3-D: when applied AMR, provides highly resolved boundaries.

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