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Incoming links: Saturn
Gas giant 2026-10-06
Past exam of the mathematics course of the University of Cambridge 2015 iii Paper 59 2 d Solution Created 2026-10-03 Updated 2026-10-06
An atmospheric thermal inversion is an altitude interval with . Absorption of incoming stellar radiation above the usual thermal-emitting layers can heat the upper gas faster than it cools, producing an inversion. In a semi-grey irradiated atmosphere, a large shortwave-to-infrared opacity ratio favors such high-altitude energy deposition; local infrared emitters and the intrinsic flux also matter.
In the Solar system, Earth and all four giant planets have well-known stratospheric inversions. The ozone layer absorbs ultraviolet sunlight on Earth; methane and photochemical hydrocarbons absorb solar radiation in the giant planets, with aerosols contributing. The giant planets are Jupiter, Saturn, Uranus and Neptune. This refers to their stratospheric temperature rise, not to the gradient at every atmospheric level.
For hot Jupiters, influential factors include the stellar flux and spectrum; the abundances of high-altitude absorbers such as titanium monoxide and vanadium monoxide; atmospheric metallicity of a giant planet and atmospheric carbon-to-oxygen ratio; thermal dissociation, atmospheric photochemistry and condensation; a atmospheric cold trap or atmospheric condensate rainout that removes absorbers; replenishment by vertical mixing; exoplanet clouds and atmospheric hazes; and heat redistribution by circulation. The ratio of visible heating to infrared cooling, rather than a single chemical species in isolation, determines whether an inversion persists.
Past exam of the mathematics course of the University of Cambridge 2015 iii Paper 59 3 b Solution Created 2026-10-03 Updated 2026-10-06
The mass-radius curve of solar-composition substellar objects reflects the transition from weak compression to pressure ionization and electron degeneracy pressure, followed by sustained hydrogen burning. A schematic joining representative object classes is:
Schematic mass-radius sequence from ice giants through gas giants and brown dwarfs to low-mass stars
. The illustration is not an age-specific numerical evolutionary model. In particular, ice giants contain much more heavy material than a solar-composition giant, so a single uniform-composition equation of state does not describe the entire joined curve.
- At the low-mass, weak-compression end, a fixed-density or fixed-composition approximation gives . Ice giants such as Neptune and Uranus have substantial water/rock-rich interiors and modest H/He envelopes; changing envelope fraction changes the radius markedly. Their heat comes from retained formation energy, contraction and radiogenic heating of heavy material. Fluid interiors generally convect, while composition stratification can impede mixing; outer radiative layers release the heat.
- Ordinary gas giants reach radii of order over a broad range around Jovian masses: an effective polytrope explains the approximate segment. Increased mass compresses material enough to offset the added volume. Cooling and Kelvin-Helmholtz contraction, with additional differentiation energy such as helium settling in Saturn, supply the intrinsic luminosity. Their deep envelopes are usually convective, with radiative photospheres.
- More massive brown dwarfs become increasingly supported by electron degeneracy pressure. The cold nonrelativistic limit gives , but finite entropy and Coulomb effects flatten actual giant/brown-dwarf curves and their radii depend on age. They cool and contract; temporary deuterium fusion occurs above a composition-dependent deuterium-burning mass near . This threshold does not cause a sharp structural kink or permanent stellar luminosity. Interiors are largely convective and surface emission is radiative.
- Near the hydrogen-burning minimum mass, roughly – or – for near-solar composition, sustained fusion prevents indefinite cooling into a degenerate object. The low-mass main-sequence star branch turns upward, with approximately over the illustrative interval. Its entropy is not constant across masses, so this branch is compatible with an approximately internal profile. Hydrogen fusion through the proton–proton chain provides energy; the lowest-mass main-sequence stars are fully convective, capped by radiative atmospheres.
Planet/brown-dwarf naming conventions and deuterium burning do not define a universal discontinuity in the mass-radius relation. Composition, age and irradiation move the curves; the hydrogen-burning transition changes the long-term energy source more fundamentally.