Limits on the Auroral Generation of H3+ in Brown Dwarf and Extrasolar Giant Planet Atmospheres with Keck/NIRSPEC
Abstract
The molecular ion H3+ is a potentially powerful tracer of the ionospheres and thermal structures of Jovian planets, but has never been detected in a planetary mass object outside of the solar system. Models predict that H3+ emission driven by EUV flux and solar wind on hot Jupiters, or by powerful aurorae on brown dwarfs, will be between 102 and 105× more intense than that of Jupiter. If optimal conditions for the production of emission do exist, the emission may be detectable by current ground-based instruments or in the near future. We present the first search for H3+ line emission in brown dwarfs with Keck/NIRSPEC L high-resolution spectroscopy. Additionally, we survey stars hosting giant planets at semi-major axes near 0.1-0.2 au, which models suggest may be the best planetary targets. No candidate H3+ emission is found. The limits we place on the emission of H3+ from brown dwarfs indicates that auroral generation of H3+ in these environments likely does not linearly scale from the processes found on Jupiter, plausibly due to deeper atmospheric penetration by precipitating auroral electrons. Detection of H3+ emission in brown dwarfs may be possible with the James Webb Space Telescope (JWST), or future thirty-meter class telescopes.
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