Spectrum and atmosphere models of irradiated transiting extrasolar giant planets
Ivan Hubeny, Adam Burrows

TL;DR
This paper models the atmospheres of irradiated transiting giant exoplanets, demonstrating that temperature inversions are necessary to fit observed secondary eclipse data and significantly affect observational signatures.
Contribution
It introduces a consistent atmospheric modeling approach showing the necessity of temperature inversions in irradiated giant planets to match observations.
Findings
Temperature inversions are required to fit secondary eclipse data.
Inversions influence planet/star contrast ratios and wavelength dependence.
Inversions correlate with stellar flux levels.
Abstract
We show that a consistent fit to observed secondary eclipse data for several strongly irradiated transiting planets demands a temperature inversion (stratosphere) at altitude. Such a thermal inversion significantly influences the planet/star contrast ratios at the secondary eclipse,their wavelength dependences, and, importantly, the day-night flux contrast during a planetary orbit. The presence of the thermal inversion/stratosphere seems to roughly correlate with the stellar flux at the planet. Such temperature inversions might caused by an upper-atmosphere absorber whose exact nature is still uncertain
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