Understanding Jupiter's Interior
arXiv:1608.02685 · doi:10.1002/2016JE005080
Abstract
This article provides an overview of how models of giant planet interiors are constructed. We review measurements from past space missions that provide constraints for the interior structure of Jupiter. We discuss typical three-layer interior models that consist of a dense central core and an inner metallic and an outer molecular hydrogen-helium layer. These models rely heavily on experiments, analytical theory, and first-principle computer simulations of hydrogen and helium to understand their behavior up to the extreme pressures ~10 Mbar and temperatures ~10,000 K. We review the various equations of state used in Jupiter models and compare them with shock wave experiments. We discuss the possibility of helium rain, core erosion and double diffusive convection may have important consequences for the structure and evolution of giant planets. In July 2016 the Juno spacecraft entered orbit around Jupiter, promising high-precision measurements of the gravitational field that will allow us to test our understanding of gas giant interiors better than ever before.
13 pages, 11 figures in J. Geophys. Research - Planets, 2016
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Cited by in corpus (6)
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- Properties of hydrogen, helium, and silicon dioxide mixtures in giant planet interiors
- A pebbles accretion model with chemistry and implications for the solar system
- Towards the same line of liquid-liquid phase transition of dense hydrogen from various theoretical predictions
- On the origin of dynamically isolated hot Earths