Can TiO Explain Thermal Inversions in the Upper Atmospheres of Irradiated Giant Planets?
David S. Spiegel, Katie Silverio, Adam Burrows (Princeton University)

TL;DR
This paper investigates whether titanium oxide (TiO) can remain in the upper atmospheres of irradiated giant exoplanets to cause thermal inversions, concluding that significant atmospheric mixing would be required, which may be unrealistic.
Contribution
The study models the vertical distribution of TiO and assesses the atmospheric mixing needed for TiO to cause thermal inversions in hot Jupiters.
Findings
TiO cannot persist in upper atmospheres without strong mixing.
Required mixing levels range from 10^7 to 10^11 cm^2/s.
Large mixing requirements challenge the TiO hypothesis for thermal inversions.
Abstract
Spitzer Space Telescope infrared observations indicate that several transiting extrasolar giant planets have thermal inversions in their upper atmospheres. Above a relative minimum, the temperature appears to increase with altitude. Such an inversion probably requires a species at high altitude that absorbs a significant amount of incident optical/UV radiation. Some authors have suggested that the strong optical absorbers titanium oxide (TiO) and vanadium oxide (VO) could provide the needed additional opacity. However, if regions of the atmosphere are cold enough for Ti and V to be sequestered into solids they might rain out and be severely depleted. With a model of the vertical distribution of a refractory species in gaseous and condensed form, we address the question of whether enough TiO (or VO) could survive aloft in an irradiated planet's atmosphere to produce a thermal inversion.…
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