Solution
ID: past-exam-of-the-mathematics-course-of-the-university-of-cambridge/2015/iii/paper-59/4/j/solution
Past exam of the mathematics course of the University of Cambridge 2015 iii Paper 59 4 j Solution by
Codex 0 Created 2026-10-03 Updated 2026-10-06
The hot-Jupiter radius inflation problem is that some strongly irradiated giant planets have radii much larger than standard age-, mass- and composition-dependent cooling models predict. Greater internal entropy generally means a larger radius at fixed mass. The two broad classes of explanation are retaining existing heat by delaying cooling and depositing additional energy into the deep planet.
- Enhanced atmospheric opacity slows radiative leakage and keeps the deep interior hot. Required enrichment or persistent cloud opacity must be compatible with composition and spectra; adding heavy material also tends to increase density. Insulation can preserve initial heat but cannot necessarily reinflate an already cooled planet.
- Layered convection in a giant planet uses a stabilizing composition gradient and double-diffusive layers to reduce heat transport. The needed gradient and layer structure must survive mixing, and their efficiency is model-dependent; very inefficient transport cannot simply be assumed for every planet.
- Tidal heating dissipates orbital or spin energy, often requiring maintained eccentricity or obliquity. Nearly circular, synchronized planets have little of the simplest eccentricity-tide power, so a pumping mechanism or different tidal configuration is needed to explain them.
- Ohmic heating of a giant planet dissipates wind-induced electric currents in a conducting, magnetized atmosphere and interior. It requires appropriate ionization, conductivity, magnetic field, wind speeds and sufficiently deep deposition; magnetic drag can limit the available mechanical power.
New to topics? Read the docs here!