Past exam of the mathematics course of the University of Cambridge 2003 iii Paper 64 3 Solution Created 2026-10-03 Updated 2026-10-14
Use , and primes for derivatives. Time dependence is , so exponential growth means . The constant mass density and incompressible velocity giveAll magnetic factors below use the source convention .
Linearizing the ideal magnetohydrodynamic momentum equation, the advective perturbation is . The magnetic force is , whose component vanishes. Thus the three component equations areIn particular the vertical equation has the pressure-gradient and magnetic signs printed in the PDF.
The incompressible ideal magnetohydrodynamic induction equation can be written . Linearizing it givesFor , these areThe term is essential: a perturbed vertical magnetic component is stretched by the background shear flow. Differentiating these amplitudes and using incompressibility also verifies .
For completeness, substitution into all three momentum equations giveswhere is the vertical vorticity amplitude. Multiplying the equation by and subtracting times the equation eliminates pressure:Therefore, away from ,This is the nonresonant reduction relevant to the instability calculation. Division at the Alfvén wave resonance would be invalid. For a concrete counterexample to an unrestricted reading, take constant , , , and , with all other amplitudes zero. Every smooth solves the original linear system, but need not vanish. These transverse resonant waves do not drive . A genuinely growing mode in a real background has complex and cannot satisfy either or on the real axis. This explains exactly when the requested reductions may be used.
On that nonresonant branch, multiply the horizontal equations by and and add. Incompressibility gives , soCombining incompressibility with vorticity, multiply its first equation by and subtract times the definition of . This givesConsequentlySubstitute this and the derivative of the displayed pressure relation into vertical momentum. Multiplication by givesExpanding the second derivative once gives exactly the requested vertical-velocity equation:
To take the discontinuous-layer limit without multiplying distributions, introduce . It is proportional to the normal displacement: the material kinematic condition is , so . Since , . The same equation becomes the displacement equation for a parallel magnetic shear flowThe physical interface condition is continuity of , because both fluids move the same interface. For constant on each side, away from resonance the coefficient is constant and nonzero, so . Requiring decay at infinity and matching yieldsThe exponent is , as in the actual PDF; the converted TeX's there is a transcription error.
Integrate the conservative displacement equation across a layer of thickness . Its undifferentiated term has an integral tending to zero, while the derivative givesEquivalently, the perturbed magnetohydrodynamic total pressure is and is continuous. With and , a nontrivial amplitude requiresThis is also the rigorous thin-layer integration of the original vertical equation, after combining the derivative terms before taking the limit.
Put and . Completing the square gives the dispersion relationFor both interface frequencies are real, so there is no exponentially growing interface mode. Above that threshold, the growing sign has growth rate . This is magnetic stabilization of an equal-density vortex sheet: magnetic tension from bending the field overcomes the kinetic shear driving Kelvin-Helmholtz instability. Equality is marginal and the strict stable condition avoids its double-root degeneracy. The case has no streamwise shear drive and has the neutral interface frequency ; the nonzero-frequency elimination should be interpreted by the original equations or a limiting displacement formulation in that case. The horizontal affects the exponential decay length through , but not the stated threshold.