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.
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CITATION STYLE
Pitman, E. B., Nichita, C. C., Patra, A. K., Bauer, A. C., Bursik, M., & Webb, A. (2003). A model of granular flows over an erodible surface. In Discrete and Continuous Dynamical Systems - Series B (Vol. 3, pp. 589–599). Southwest Missouri State University. https://doi.org/10.3934/dcdsb.2003.3.589
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