2018
DOI: 10.3847/1538-3881/aad564
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Detectability of Biosignatures in Anoxic Atmospheres with the James Webb Space Telescope: A TRAPPIST-1e Case Study

Abstract: The James Webb Space Telescope (JWST) may be capable of finding biogenic gases in the atmospheres of habitable exoplanets around low mass stars. Considerable attention has been given to the detectability of biogenic oxygen, which could be found using an ozone proxy, but ozone detection with JWST will be extremely challenging, even for the most favorable targets. Here, we investigate the detectability of biosignatures in anoxic atmospheres analogous to those that likely existed on the early Earth. Arguably, suc… Show more

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Cited by 146 publications
(164 citation statements)
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“…We used Pan-dExo (Batalha et al 2017) to generate the wavelength grid and noise for the NIRSpec Prism (0.6 -5.3 µm), NIRSpec G395M (2.87 -5.10 µm), NIRSpec G235M (1.66 -3.07 µm) and NIRSpec G140M (0.97 -1.84 µm), this is done for the integration time of the secondary eclipse of WASP-43b. For the NIRSpec Prism (nominal resolving power ∼100) we use the resolution of the largest bin step as shown in Krissansen-Totton et al (2018) and for the different NIRSpec gratings (nominal resolving power ∼1000) we use a resolution of R=100.…”
Section: Application To Nirspecmentioning
confidence: 99%
“…We used Pan-dExo (Batalha et al 2017) to generate the wavelength grid and noise for the NIRSpec Prism (0.6 -5.3 µm), NIRSpec G395M (2.87 -5.10 µm), NIRSpec G235M (1.66 -3.07 µm) and NIRSpec G140M (0.97 -1.84 µm), this is done for the integration time of the secondary eclipse of WASP-43b. For the NIRSpec Prism (nominal resolving power ∼100) we use the resolution of the largest bin step as shown in Krissansen-Totton et al (2018) and for the different NIRSpec gratings (nominal resolving power ∼1000) we use a resolution of R=100.…”
Section: Application To Nirspecmentioning
confidence: 99%
“…We acknowledge, up front, that this may not be a physically plausible scenario due to the vastly different incident spectral energy distribution. However, given the overwhelming number of unknowns involved in self-consistent planetary atmosphere modeling (e.g., star-planet interactions, surface fluxes, formation conditions, bulk elemental composition, 3D atmospheric dynamical effects, cloud micro-physics, dynamical evolution/history) we simply choose to treat our atmosphere as "Earth-like" (as has also been done in previous works, Morley et al (2017); Krissansen-Totton et al (2018)).…”
Section: Transmission Forward Modelmentioning
confidence: 99%
“…Utilizing a combination of NIR-Spec PRISM and MIRI-LRS, they conclude that O 3 , at Earth-like abundances, would be detectable on planets 1c and 1d with 30 transits on each instrument. Also utilizing an atmospheric retrieval analysis, Krissansen-Totton et al (2018) analyzed the detectability of the CO 2 +CH 4 disequilibrium biosignature, suspected to have been present in Earth's early atmosphere when the abundances of each were significantly enhanced compared to modern-day values.…”
Section: Introductionmentioning
confidence: 99%
“…We also expect to be able to determine atmospheric properties of smaller rocky planets orbiting M-dwarf host stars. It may in certain cases be possible to detect atmospheric biosignatures, but this will be challenging for JWST (Krissansen-Totton et al 2018;Lustig-Yaeger et al 2019). Unfortunately the characterization of the atmosphere of an Earth-like planet around a Sun-like star will be beyond the reach of JWST.…”
Section: Rv Observations To Better Determine the Planet Massesmentioning
confidence: 99%