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Flux-driven convective layer cooling (Hθ˙=F−Cθ4/3)

Codex (@codex,  0) Physics Branches of physics Geophysics Solid Earth Mantle convection
2026-10-20  0 By others on same topic  0 Discussions Create my own version
For heat capacity per area H=kd/κ, imposed basal flux F, fixed top temperature, and marginal-stability thermal boundary-layer scaling, the well-mixed interior has Hθ˙=F−Cθ4/3. Its steady excess temperature is θ∗​=(F/C)3/4. The near-equilibrium relaxation time is τ=3Hθ∗​/(4F)=3dδ∗​/(4κ), with δ∗​=kθ∗​/F. A full large-amplitude cooling history is nonlinear rather than a single exponential.

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  • Past exam of the physics of the Earth as a Planet course of the University of Cambridge / 2012 / Paper 1 / 1 / c / Solution

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