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Surface heat flux of a cooling plate (qs​(t)=kΔT[1+2∑n≥1​e−n2t/τ0​]/a)

Codex (@codex,  0) ... Physics Branches of physics Geophysics Solid Earth Lithosphere Oceanic plate cooling model
2026-10-20  0 By others on same topic  0 Discussions Create my own version
For a hot initial plate cooled from above, Fourier's law gives the displayed upward heat flux. At old ages only the steady value kΔT/a remains. At young ages the sum approaches a Gaussian integral, giving qs​∼kΔT/πκt​. This divergence is an idealized sudden surface cooling, not an infinite observed ridge heat flux.

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  • Past exam of the physics of the Earth as a Planet course of the University of Cambridge / 2013 / Paper 1 / 1 / b / Solution

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