1. Transit Lyman-α signatures of terrestrial planets in the habitable zones of M dwarfs
- Author
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Manuel Güdel, I. F. Shaikhislamov, Helmut Lammer, Kristina G. Kislyakova, Ernst A. Dorfi, Maxim L. Khodachenko, Mats Holmström, Nikolai V. Erkaev, and Petra Odert
- Subjects
Physics ,010504 meteorology & atmospheric sciences ,Astronomy and Astrophysics ,Astrophysics::Cosmology and Extragalactic Astrophysics ,Astrophysics ,01 natural sciences ,Atmosphere ,Stars ,13. Climate action ,Space and Planetary Science ,Planet ,0103 physical sciences ,Astrophysics::Solar and Stellar Astrophysics ,Terrestrial planet ,Astrophysics::Earth and Planetary Astrophysics ,Transit (astronomy) ,010303 astronomy & astrophysics ,Circumstellar habitable zone ,Space Telescope Imaging Spectrograph ,Astrophysics - Earth and Planetary Astrophysics ,0105 earth and related environmental sciences ,Line (formation) - Abstract
We modeled the transit signatures in the Lya line of a putative Earth-sized planet orbiting in the HZ of the M dwarf GJ436. We estimated the transit depth in the Lya line for an exo-Earth with three types of atmospheres: a hydrogen-dominated atmosphere, a nitrogen-dominated atmosphere, and a nitrogen-dominated atmosphere with an amount of hydrogen equal to that of the Earth. We calculated the in-transit absorption they would produce in the Lya line. We applied it to the out-of-transit Lya observations of GJ 436 obtained by the HST and compared the calculated in-transit absorption with observational uncertainties to determine if it would be detectable. To validate the model, we also used our method to simulate the deep absorption signature observed during the transit of GJ 436b and showed that our model is capable of reproducing the observations. We used a DSMC code to model the planetary exospheres. The code includes several species and traces neutral particles and ions. At the lower boundary of the DSMC model we assumed an atmosphere density, temperature, and velocity obtained with a hydrodynamic model for the lower atmosphere. We showed that for a small rocky Earth-like planet orbiting in the HZ of GJ436 only the hydrogen-dominated atmosphere is marginally detectable with the STIS/HST. Neither a pure nitrogen atmosphere nor a nitrogen-dominated atmosphere with an Earth-like hydrogen concentration in the upper atmosphere are detectable. We also showed that the Lya observations of GJ436b can be reproduced reasonably well assuming a hydrogen-dominated atmosphere, both in the blue and red wings of the Lya line, which indicates that warm Neptune-like planets are a suitable target for Lya observations. Terrestrial planets can be observed in the Lya line if they orbit very nearby stars, or if several observational visits are available., Comment: 17 pages, 12 figures, accepted for publication in Astronomy & Astrophysics
- Published
- 2019
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