H2O abundances in the atmospheres of three hot Jupiters
Nikku Madhusudhan (IoA, Cambridge), Nicolas Crouzet (Dunlap, Institute), Peter R. McCullough (STScI), Drake Deming (U. Maryland),, Christina Hedges (IoA, Cambridge)

TL;DR
This study measures water vapor in three hot Jupiter atmospheres using HST data, providing insights into their composition and formation, with the most precise water measurement in an exoplanet to date.
Contribution
First precise measurement of H2O in HD 209458b, revealing sub-solar water abundance and advancing understanding of hot Jupiter atmospheres and formation conditions.
Findings
HD 189733b and HD 209458b have nearly solar or sub-solar H2O abundances.
WASP-12b's H2O abundance is not well constrained by current data.
HD 209458b shows the most precise sub-solar H2O measurement in an exoplanet to date.
Abstract
The core accretion theory for giant planet formation predicts enrichment of elemental abundances in planetary envelopes caused by runaway accretion of planetesimals, which is consistent with measured super-solar abundances of C, N, P, S, Xe, and Ar in Jupiter's atmosphere. However, the abundance of O which is expected to be the most dominant constituent of planetesimals is unknown for solar system giant planets, owing to the condensation of water in their ultra-cold atmospheres, thereby posing a key unknown in solar system formation. On the other hand, hundreds of extrasolar hot Jupiters are known with very high temperatures (>~1000 K) making them excellent targets to measure H2O abundances and, hence, oxygen in their atmospheres. We constrain the atmospheric H2O abundances in three hot Jupiters (HD 189733b, HD 209458b, and WASP-12b), spanning a wide temperature range (1200-2500 K),…
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