Geostrophic turbulence with a magnetic field
The project is an extension of the work on f-plane magnetohydrodynamic (MHD) turbulence and its consequences on momentum transport. A somewhat detailed overview is given, with the physical mechanisms explained. The quasi-geostrophic equations, so well known in the Geophysical Fluid Dynamics (GFD) community, is derived with the Lorentz force present. The two-layer model is proposed as a simplified model for our studies. Progress with magnetically influenced barotropic and baroclinic instabilities are given, and some proposed future work concludes the document.