Atmospheric Circulation of Close-in Extrasolar Giant Planets. I. Global, Barotropic, Adiabatic Simulations

Details Atmospheric Circulation of Close-in Extrasolar Giant Planets. I. Global, Barotropic, Adiabatic Simulations Atmospheric Circulation of Close-in Extrasolar Giant Planets. I. Global, Barotropic, Adiabatic Simulations

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008apj...675..817c&link_type=abstract

The Astrophysical Journal, Volume 675, Issue 1, pp. 817-845.

Astronomy and Astrophysics

Astronomy

34

Stars: Planetary Systems, Planets And Satellites: General, Stars: Atmospheres, Turbulence

Scientific paper

We present results from a set of over 300 pseudospectral simulations of atmospheric circulation on extrasolar giant planets with circular orbits. The simulations are of high enough resolution (up to 341 total and sectoral modes) to resolve small-scale eddies and waves, required for reasonable physical accuracy. In this work, we focus on the global circulation pattern that emerges in a shallow, ``equivalent barotropic,'' turbulent atmosphere on both tidally synchronized and unsynchronized planets. A full exploration of the large physical and numerical parameter space is performed to identify robust features of the circulation. For some validation, the model is first applied to solar system giant planets. For extrasolar giant planets with physical parameters similar to HD 209458b-a presumably synchronized extrasolar giant planet, representative in many dynamical respects-the circulation is characterized by the following features: (1) a coherent polar vortex that revolves around the pole in each hemisphere; (2) a low number (typically two or three) of slowly varying, broad zonal (east-west) jets that form when the maximum jet speed is comparable to, or somewhat stronger than, those observed on the planets in the solar system; and (3) a motion-associated temperature field, whose detectability and variability depend on the strength of the net heating rate and the global rms wind speed in the atmosphere. In many ways, the global circulation is Earth-like, rather than Jupiter-like. However, if extrasolar giant planets rotate faster and are not close-in (therefore not synchronized), their circulations become more Jupiter-like, for Jupiter-like rotation rates.

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