MHD Heat Transfer in a Magma Convection Model

MHD Heat Transfer in a Magma Convection Model#

Domain: A 2D representation of the Earth’s mantle.

Boundary Conditions:

  • Top Surface: Heat flux condition.

  • Bottom Surface: Insulated conditions.

  • Side Boundaries: No-slip conditions for velocity.

Initial Conditions:

  • Initial temperature distribution representing the initial state of the mantle.

These test cases provide a starting point for simulating MHD Heat Transfer. Actual applications may involve more complex geometries, additional physical effects, and tailored boundary conditions based on specific scenarios.