Search for Rayleigh scattering in the atmosphere of GJ1214b
Ernst J.W. de Mooij, Matteo Brogi, Remco J. de Kok, Ignas A.G Snellen,, Bryce Croll, Ray Jayawardhana, Henk Hoekstra, Gilles P.P.L. Otten, David H., Bekkers, Sebastiaan Y. Haffert, Josha. J. van Houdt

TL;DR
This study investigates the atmosphere of GJ1214b by measuring its transit depth across optical wavelengths, finding no significant Rayleigh scattering signature and supporting a water-dominated, low-scale-height atmosphere.
Contribution
First optical measurements of GJ1214b's transit depth across multiple telescopes, providing evidence against Rayleigh scattering and supporting a water-rich atmosphere.
Findings
No significant Rayleigh scattering detected.
Optical data consistent with a flat transmission spectrum.
Supports a water-dominated, low-scale-height atmospheric model.
Abstract
We investigate the atmosphere of GJ1214b, a transiting super-Earth planet with a low mean density, by measuring its transit depth as a function of wavelength in the blue optical portion of the spectrum. It is thought that this planet is either a mini-Neptune, consisting of a rocky core with a thick, hydrogen-rich atmosphere, or a planet with a composition dominated by water. Most observations favor a water-dominated atmosphere with a small scale-height, however, some observations indicate that GJ1214b could have an extended atmosphere with a cloud layer muting the molecular features. In an atmosphere with a large scale-height, Rayleigh scattering at blue wavelengths is likely to cause a measurable increase in the apparent size of the planet towards the blue. We observed the transit of GJ1214b in the B-band with the FOcal Reducing Spectrograph (FORS) at the Very Large Telescope (VLT) and…
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