Ionization of Extrasolar Giant Planet Atmospheres

Details Ionization of Extrasolar Giant Planet Atmospheres Ionization of Extrasolar Giant Planet Atmospheres

Oct 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010apj...722..178k&link_type=abstract

The Astrophysical Journal, Volume 722, Issue 1, pp. 178-187 (2010).

Astronomy and Astrophysics

Astronomy

2

Hydrodynamics, Magnetohydrodynamics: Mhd, Planets And Satellites: General, Plasmas, Turbulence

Scientific paper

Many extrasolar planets orbit close in and are subject to intense ionizing radiation from their host stars. Therefore, we expect them to have strong, and extended, ionospheres. Ionospheres are important because they modulate escape in the upper atmosphere and can modify circulation, as well as leave their signatures, in the lower atmosphere. In this paper, we evaluate the vertical location Z_I and extent D_I of the EUV ionization peak layer. We find that Z_I ≈ 1-10 nbar—for a wide range of orbital distances (a = 0.047-1 AU) from the host star—and D_I/H_p ≳ 15, where Hp is the pressure scale height. At Z_I, the plasma frequency is ~80-450 MHz, depending on a. We also study global ion transport, and its dependence on a, using a three-dimensional thermosphere-ionosphere model. On tidally synchronized planets with weak intrinsic magnetic fields, our model shows only a small, but discernible, difference in electron density from the dayside to the nightside (~9 × 1013 m-3 to ~2 × 1012 m-3, respectively) at Z_I. On asynchronous planets, the distribution is essentially uniform. These results have consequences for hydrodynamic modeling of the atmospheres of close-in extrasolar giant planets.

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