A Global Simulation of the Dynamo, Zonal Jets, and Vortices on Saturn

Abstract

The fluid dynamics in planet Saturn gives rise to alternating east-west jet streams, large cyclonic and anticyclonic vortices, and a dipole-dominant magnetic field which is highly axisymmetric about the planetary rotation axis. Modelling these features in a self-consistent manner is crucial for understanding the dynamics of Saturn's interior and atmosphere. Here we report a turbulent high-resolution dynamo simulation in a spherical shell which produces these features simultaneously for the first time. A crucial model ingredient is a long-hypothesised stably stratified layer (SSL), sandwiched between a deep metallic hydrogen layer and an outer low-conductivity molecular layer, born out of limited solubility of Helium inside metallic Hydrogen at certain depths. The model spontaneously produces polar cyclones and significant low and mid latitude jet stream activities in the molecular layer. The off-equatorial low-latitude jet streams partially penetrate into the SSL and interact with the magnetic field. This helps to axisymmetrize the magnetic field about the rotation axis and convert some of the poloidal magnetic field to toroidal field, which appears as two global magnetic energy rings surrounding the deeper dynamo region. The simulation also mimics a distinctive dip in the fifth spherical harmonic in Saturn's magnetic energy spectrum as inferred from the Cassini Grand Finale measurements. Our model highlights the role of an SSL in shaping the fluid dynamical and magnetic features of giant planets, as exemplified at Saturn.

arXiv comment17 pages, 8 figures. Published in ApJ

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• A Possible Mechanism to Explain the Prograde Equatorial Jet of a Jupiter-like Gaseous Giant