Ideal magnetorotational dispersion relation 2026-10-05
For a vertical magnetic field in a homogeneous shearing sheet, a horizontal normal mode with growth rate and vertical Alfvén frequency satisfiesThe two roots for are real. For , a growing magnetic mode exists precisely when . Magnetic tension is strong enough to couple radially displaced elements, yet weak enough to allow their separation to increase. Ogilvie's lecture on magnetorotational instability derives this relation and its finite-thickness boundary conditions.
Past exam of the mathematics course of the University of Cambridge 2019 iii Paper 321 3 c Solution Created 2026-10-03 Updated 2026-10-05
The horizontally invariant magnetized shearing-sheet equations are linear in the horizontal fields, so perturbations about the equilibrium satisfy the same equations. The fixed surface boundary conditions require at . Choose a normal mode withwhere the vertical wavenumber is , . With the Alfvén frequencythe four amplitude equations becomeEliminating the velocities leavesA nonzero amplitude requires the determinant of this system to vanish, yielding the ideal magnetorotational dispersion relationEquivalently, with ,As a quadratic equation for , its discriminant is . If , its constant term is negative, so one root is positive and there is an exponentially growing mode. If , both the constant term and the coefficient of are positive, giving two negative roots and only oscillatory modes. Equality is marginal.
The lowest allowed vertical wavenumber, , is the last to be stabilized as increases. Therefore the finite-thickness magnetorotational instability criterion isThere is also a vertically uniform velocity mode with zero magnetic perturbation; for the usual orbitally stable regime , it is just stable epicyclic motion. For , that uniform mode is already hydrodynamically unstable, independently of the magnetic criterion. At it is marginal. The criterion above concerns the magnetic modes.