Temporal variations in the evaporating atmosphere of the exoplanet HD 189733b
A. Lecavelier des Etangs, V. Bourrier, P.J. Wheatley, H. Dupuy, D., Ehrenreich, A. Vidal-Madjar, G. H\'ebrard, G.E. Ballester, J.-M. D\'esert, R., Ferlet, D.K. Sing

TL;DR
This study presents spectrally resolved Lyman-alpha transit observations of exoplanet HD 189733b, revealing significant temporal variations in its evaporating atmosphere and suggesting interactions with stellar wind and energy input changes.
Contribution
First spectrally resolved observations showing temporal variability in the atmospheric escape of HD 189733b and evidence of stellar wind interactions affecting atmospheric conditions.
Findings
Detected atmospheric hydrogen only in the second epoch
Observed high-velocity hydrogen absorption requiring stellar wind interactions
Linked atmospheric variations to stellar activity such as X-ray flares
Abstract
Atmospheric escape has been detected from the exoplanet HD 209458b through transit observations of the hydrogen Lyman-alpha line. Here we present spectrally resolved Lyman-alpha transit observations of the exoplanet HD 189733b at two different epochs. These HST/STIS observations show for the first time, that there are significant temporal variations in the physical conditions of an evaporating planetary atmosphere. While atmospheric hydrogen is not detected in the first epoch observations, it is observed at the second epoch, producing a transit absorption depth of 14.4+/-3.6% between velocities of -230 to -140 km/s. Contrary to HD 209458b, these high velocities cannot arise from radiation pressure alone and require an additional acceleration mechanism, such as interactions with stellar wind protons. The observed absorption can be explained by an atmospheric escape rate of neutral…
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