Abstract
We present a framework for modeling a dry geophysical mass of granular material - a debris or volcanic avalanche or landslide - flowing over an erodible surface. We also describe a computing environment that incorporates topographical data into a parallel, adaptive mesh computational algorithm that solves the model equations.
| Original language | English |
|---|---|
| Pages (from-to) | 589-599 |
| Number of pages | 11 |
| Journal | Discrete and Continuous Dynamical Systems - Series B |
| Volume | 3 |
| Issue number | 4 |
| DOIs | |
| State | Published - Nov 2003 |
Keywords
- Computational methods
- Geological problems
- Numerical approximation of solutions
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