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Water, Methane, and Carbon Dioxide Present in the Dayside Spectrum of the Exoplanet HD 209458b (0908.4010v1)

Published 27 Aug 2009 in astro-ph.EP and astro-ph.SR

Abstract: Using the NICMOS instrument on the Hubble Space Telescope, we have measured the dayside spectrum of HD 209458b between 1.5--2.5 microns. The emergent spectrum is dominated by features due to the presence of methane (CH4) and water vapor (H2O), with smaller contributions from carbon dioxide (CO2). Combining this near-infrared spectrum with existing mid-infrared measurements shows the existence of a temperature inversion and confirms the interpretation of previous photometry measurements. We find a family of plausible solutions for the molecular abundance and detailed temperature profile. Observationally resolving the ambiguity between abundance and temperature requires either (1) improved wavelength coverage or spectral resolution of the dayside emission spectrum, or (2) a transmission spectrum where abundance determinations are less sensitive to the temperature structure.

Citations (218)

Summary

  • The paper demonstrates the spectroscopic detection of water vapor and methane, confirming a temperature inversion in HD 209458b's atmosphere.
  • The methodology utilizes HST NICMOS with decorrelation of instrumental variables over five orbits to produce a high-precision near-infrared spectrum.
  • The findings encourage model adaptations and emphasize the need for further observations with instruments like JWST to refine atmospheric profiles.

Analysis of Molecular Detection in the Atmosphere of HD~209458b

The research presented by Swain et al. focuses on the composition and structure of the atmosphere of the exoplanet HD~209458b, employing the Near Infrared Camera and Multi-Object Spectrometer (NICMOS) on the Hubble Space Telescope (HST) for spectrum acquisition. This paper aims to extend our understanding of hot-Jupiter atmospheres, notably through the first spectroscopic detection of molecules in the atmosphere of HD~209458b.

Observational and Methodological Framework

The authors conducted their observations over five consecutive HST orbits, capturing near-infrared spectra ranging from 1.5 to 2.5 micrometers. Notably, the NICMOS instrument was utilized in imaging-spectroscopy mode, achieving a spectral resolution of approximately R = 40. This methodological choice allows for a detailed spectroscopic analysis of the radiative features arising from the planetary atmosphere, thereby supporting the identification of molecular constituents.

The analytical approach is predicated on a decorrelation of instrumental variables against spectrophotometric light curves, facilitating a reduced-noise spectrum with higher precision. The data calibration process was bolstered through contemporaneous observations via the MOST satellite, providing a reliable baseline against which variations in system brightness could be measured.

Key Findings and Interpretation

From the resulting spectrum, pronounced features attributable to methane (CH₄) and water vapor (H₂O) dominate, with carbon dioxide (CO₂) presenting more subtle absorptive characteristics. Coupled with prior mid-infrared Spitzer observations, the findings indicate a temperature inversion in the atmosphere, marking a divergence from uniform radiative profiles. The researchers evaluate a family of temperature and molecular profiles consistent with these measurements.

This identified temperature inversion occurs between pressures of 0.1 to 0.0001 bar, akin to stratospheric conditions seen in planetary atmospheres. The discovery of a temperature inversion coincides with the hypothesis that an additional absorbing molecule, ostensibly CO₂, contributes to the local atmospheric heating.

Comparative and Theoretical Implications

Comparative analysis draws on data from another well-studied hot-Jupiter, HD~189733b. While both planets exhibit signatures of similar molecular species, the abundance of CH₄ in HD~209458b's atmosphere is notably higher, implying distinct chemical and thermal atmospheric processes. This work suggests that while existing models adequately describe broad trends in exoplanetary atmospheres, the specific optical depths and molecular abundances provide critical insights into atmospheric dynamics and chemical compositions.

The implications of these findings are multifaceted:

  • Model Adaptations: The presence of a temperature inversion challenges erstwhile one-dimensional atmospheric models, necessitating considerations of vertical mixing and potential radiative equilibrium deviations.
  • Future Observations: Enhanced spectral coverage via instruments like the James Webb Space Telescope (JWST) could refine molecular abundance estimates and further elucidate pressure-temperature profiles.
  • Atmospheric Dynamics: The interaction of temperature inversion dynamics with chemical processes could inform broader planetary atmospheric studies, influencing our understanding of planetary formation and evolution.

Conclusion

Swain et al. contribution to the domain of exoplanetary atmospheric research is pivotal, setting a benchmark in molecular spectroscopy of exoplanets. While outlining significant discoveries regarding HD~209458b's atmospheric constituents, the paper underscores the complexity of atmospheric processes in hot-Jupiters and the potential variability that could characterize their radiative and chemical environments. As observational techniques advance, this work provides a foundational reference for future inquiries into atmospheric inversions and molecular detections in similar astronomical bodies.

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