
MILEVA
Lead developerMantle Interaction and Lithospheric Evolution in Viscous Annuli
A finite-volume mantle-convection code in Julia.
MILEVA simulates thermal and compositional convection in Earth-like and planetary mantles. It solves the coupled Stokes, energy and composition equations on a staggered finite-volume grid, with velocities on cell faces and pressure at cell centres, while temperature and composition ride on Lagrangian markers.
- Language
- Julia
- Method
- Finite volume, staggered grid
- Transport
- Lagrangian markers
- Geometry
- 2-D spherical and cylindrical annulus · 3-D spherical chunk and Yin-Yang sphere