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Characterising a World Within the Hot Neptune Desert: Transit Observations of LTT 9779 b with HST WFC3

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arxiv 2306.13645 v1 pith:QAQREEK5 submitted 2023-06-23 astro-ph.EP

classification astro-ph.EP
keywords atmosphericevidenceobservationsplanetsigmaatmospheredatadesert
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abstract

We present an atmospheric analysis of LTT 9779 b, a rare planet situated in the hot Neptune desert, that has been observed with HST WFC3 G102 and G141. The combined transmission spectrum, which covers 0.8 - 1.6 $\mu$m, shows a gradual increase in transit depth with wavelength. Our preferred atmospheric model shows evidence for H$_{\rm 2}$O, CO$_{\rm 2}$ and FeH with a significance of 3.1 $\sigma$, 2.4 $\sigma$ and 2.1 $\sigma$, respectively. In an attempt to constrain the rate of atmospheric escape for this planet, we search for the 1.083 $\mu$m Helium line in the G102 data but find no evidence of excess absorption that would indicate an escaping atmosphere using this tracer. We refine the orbital ephemerides of LTT 9779 b using our HST data and observations from TESS, searching for evidence of orbital decay or apsidal precession, which is not found. The phase-curve observation of LTT 9779 b with JWST NIRISS should provide deeper insights into the atmosphere of this planet and the expected atmospheric escape might be detected with further observations concentrated on other tracers such as Lyman $\alpha$.

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Cited by 2 Pith papers

Reviewed papers in the Pith corpus that reference this work. Sorted by Pith novelty score. Full citation record

  1. Highly reflective white clouds on the western dayside of an exo-Neptune

    astro-ph.EP 2025-01 conditional novelty 7.0 of 10

    Phase-resolved JWST spectroscopy of LTT 9779b reveals a 3.1 sigma east-west albedo asymmetry, with reflective silicate clouds on the western dayside and a symmetric thermal phase curve.

  2. Instrumentation prospects for rocky exoplanet atmospheres studies with high resolution spectroscopy

    astro-ph.EP 2025-05 conditional novelty 5.0 of 10

    Higher spectral resolution (R=300,000) materially reduces the exposure time needed to detect oxygen A-band absorption in hazy, cloudy exoplanet atmospheres relative to R=100,000.

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