Physics
Scientific paper
Aug 2007
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007pepi..163...52k&link_type=abstract
Physics of the Earth and Planetary Interiors, Volume 163, Issue 1-4, p. 52-68.
Physics
13
Magma Migration, Mid-Oceanic Ridge Processes, Tectonophysics, Convection Currents And Mantle Plumes, Finite Volume Methods, Numerical Simulation, Solution Of Equations
Scientific paper
Geodynamics simulations are characterized by rheological nonlinearity, localization, three-dimensional effects, and separate but interacting length scales. These features represent a challenge for computational science. We discuss how a leading software framework for advanced scientific computing (the Portable Extensible Toolkit for Scientific Computation, PETSc) can facilitate the development of geodynamics simulations. To illustrate our use of PETSc, we describe simulations of (i) steady-state, non-Newtonian passive flow and thermal structure beneath a mid-ocean ridge, (ii) magmatic solitary waves in the mantle, and (iii) the formation of localized bands of high porosity in a two-phase medium being deformed under simple shear. We highlight two supplementary features of PETSc, structured storage of application parameters and self-documenting output, that are especially useful for geodynamics simulations.
Coon E. T.
Katz Richard F.
Knepley Matthew G.
Smith Brett
Spiegelman Marc
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