Exploring the ultrahot Neptune LTT 9779 b with CRIRES+. Non-detection of helium transmission spectra and detection of HO on the dayside
arXiv:2610.07202
Abstract
Ultrahot Neptunes reside in the most extreme irradiation regime of the hot Neptune desert and remain challenging targets for atmospheric characterization because of their low planet-to-star flux ratios. We present high-resolution transit and dayside thermal emission spectroscopy of the ultrahot Neptune LTT 9779 b obtained with CRIRES, to probe atmospheric escape and dayside molecular emission. No significant absorption is detected in the metastable He I nm triplet during transit, yielding a upper limit of 0.45% on the excess helium absorption depth and supporting previous non-detections that suggest weak ongoing atmospheric escape. For the dayside emission spectra in the band, our cross-correlation analysis reveals an absorption signal and a tentative feature, with the combined signal reaching a detection significance of . Both the CRIRES and previous JWST data favor a non-inverted temperature structure, providing no evidence of a thermal inversion on the planetary dayside. We further perform a joint atmospheric retrieval combining the CRIRES high-resolution spectra with JWST/NIRISS SOSS secondary-eclipse observations. The joint retrieval yields a low abundance, while the abundance remains weakly constrained. The inferred planetary equatorial rotational velocity, , is consistent within with the synchronous rotation velocity expected for a tidally locked planet (). However, the large uncertainties prevent us from placing strong constraints on the planet's rotation state. Future phase-resolved CRIRES observations with broader orbital-phase coverage and higher signal-to-noise ratios would improve the abundance constraints and probe the atmospheric dynamics of this rare ultrahot Neptune.
arXiv comment19 pages, 13 figures. Accepted for publication in A&A