Near-UV transit photometry of HAT-P-32 b with the LBT: Silicate aerosols in the planetary atmosphere
Matthias Mallonn, Hannah R. Wakeford

TL;DR
This study presents the first high-quality ground-based U-band transit observation of exoplanet HAT-P-32 b, revealing a scattering slope in its atmosphere likely caused by magnesium silicate aerosols, and compares this feature across multiple exoplanets.
Contribution
It provides the best ground-based U-band transit data of an exoplanet and introduces a spectral index to compare aerosol scattering features across different planets.
Findings
Detected a clear scattering slope indicating aerosols in HAT-P-32 b's atmosphere.
Most likely magnesium silicate aerosols larger than 0.1 micrometer are responsible.
The scattering feature is typical compared to other exoplanets in the sample.
Abstract
Broad-band exoplanet transit photometry can characterize the planetary atmosphere when observed at multiple selected filters. This observing technique can reveal gradients in the spectra of extrasolar planets, for example the slope of decreasing opacity from short to long optical wavelengths caused by aerosol scattering. In this work we observed a transit of the hot Jupiter HAT-P-32 b in the shortest wavelength possible from the ground using the Large Binocular Telescope (LBT). The data comprise the best-quality ground-based U-band taken so far of an exoplanet transit. Compared to broad-band observations of intermediate and long optical wavelength published previously, a clear scattering slope in the planetary transmission spectrum is revealed. Most likely, the scattering particles are magnesium silicate aerosols larger than 0.1 micrometer. We define a spectral index to compare this…
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