An empirical infrared transit spectrum of Earth: opacity windows and biosignatures

Evelyn J. R. Macdonald; Nicolas B. Cowan

doi:10.1093/mnras/stz2047

paper

An empirical infrared transit spectrum of Earth: opacity windows and biosignatures

arXiv:1908.10873 · doi:10.1093/mnras/stz2047

Abstract

The Atmospheric Chemistry Experiment's Fourier Transform Spectrometer on the SCISAT satellite has been measuring infrared transmission spectra of Earth during Solar occultations since 2004. We use these data to build an infrared transit spectrum of Earth. Regions of low atmospheric opacity, known as windows, are of particular interest, as they permit observations of the planet's lower atmosphere. Even in the absence of clouds or refraction, imperfect transmittance leads to a minimum effective thickness of $h_{min} \approx 4$ km in the 10--12 $μ$ m opacity window at a spectral resolution of $R = 1 0^{3}$ . Nonetheless, at $R = 1 0^{5}$ , the maximum transmittance at the surface is around 70%. In principle, one can probe the troposphere of an Earth-like planet via high-dispersion transit spectroscopy in the mid-infrared; in practice aerosols and/or refraction likely make this impossible. We simulate the transit spectrum of an Earth-like planet in the TRAPPIST-1 system. We find that a long-term near-infrared campaign with JWST could readily detect CO $_{2}$ , establishing the presence of an atmosphere. A mid-IR campaign or longer NIR campaign would be more challenging, but in principle could detect H $_{2}$ O and the biosignatures O $_{3}$ and CH $_{4}$ .

arXiv comment9 pages, 7 figures; updated figures 3, 6, and 7 to relabel the CO $_{2}$ feature at 2.7 $μ$ m; water vapour is more difficult to detect than originally stated

An empirical infrared transit spectrum of Earth: opacity windows and biosignatures

Abstract

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