Solution

ID: past-exam-of-the-physics-of-the-earth-as-a-planet-course-of-the-university-of-cambridge/2012/paper-1/1/c/solution

For flux-driven convective layer cooling, use with the same unspecified coefficient as in (b). The steady heat balance gives
The corresponding boundary-layer thickness is
Set and expand the heat loss to first order. Since ,
This is the near-equilibrium relaxation time. The full equation is nonlinear, so an arbitrary large initial temperature departure need not decay as one exponential. Positive heat loss derivative makes the steady state stable. In particular, scales with , rather than , because convection shortens the effective heat-transport distance to the boundary layer.

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