Abstract:
Context: Over 5,000 exoplanets have been discovered to date, yet our
knowledge of their atmospheres is still quite limited, and we have not yet
identified any truly habitable exoplanets. It is the high time to characterize
the atmospheres of Earth-like planets, especially as we enter an era of
ambitious, big missions such as the Roman Space Telescope, the Thirty Meter
Telescope, HabEx, the Extremely Large Telescope, and the Habitable
Worlds Observatory (HWO). These groundbreaking missions are poised to
significantly enhance our understanding and bring us closer to discovering
potentially habitable worlds.
Aim: Our goal is to characterize the atmospheres of terrestrial exoplanets
by calculating their reflected spectra, transmission spectra, and polarization
phase curves. For the reflection spectra, we considered both present
and prebiotic Earth-like exoplanets orbiting stars of F, G, K, and M spectral
types, as well as nine known terrestrial exoplanets. The transmission
spectra are modeled for present and prebiotic Earth-like exoplanets using
the Beer-Bouguer-Lambert’s law and a general law of multiple scattering,
which accounts for diffused radiation. We also model the polarization phase
curves of terrestrial exoplanets orbiting Sun-like stars. Various planetary
surface types were considered, including water worlds, present and prebiotic
Earth-like surfaces, and different sky conditions, such as clear and
cloudy atmospheres. Additionally, we modeled atmospheres with increased
greenhouse gas abundances. Methodology: The reflected spectra and geometric albedo is computed
by solving the equation applicable for multiple scattering radiative transfer
problem. The atmospheric abundance is assumed to be analogous to that
of the present Earth-like exoplanets. The Temperature - Pressure profiles
for the known exoplanets are derived using hydrostatic equilibrium and
the energy balance equation. The transmission spectra is calculated using
Beer-Bouguer-Lambert’s law as well as using multiple scattering radiative
transfer equation. We numerically solve the 3D vector radiative transfer
equations to calculate the phase curves of albedo and disk-integrated polarization
by using appropriate scattering phase matrices and integrating
the local Stokes vectors over the illuminated part of the planetary disks
along the line of sight.
Results: Firstly, we present the reflected spectra and the geometric
albedo for the present and prebiotic Earth-like exoplanets orbiting around
F, G, K and M spectral types of stars and also for the nine known terrestrial
exoplanets. We note the effect of the globally averaged surface albedo,
clouds and the greenhouse gases abundance on the reflectivity. Secondly,
we present the transmission spectra for Earth-like exoplanets, both with
and without diffused scattering. We see the effect of the clouds on the
transmission spectra and note the absorption lines of the bio-molecules
present in the planetary atmospheres. Our models demonstrate that the
effect of the diffusely transmitted radiation can be significant, especially in
the atmospheres with clouds. Thirdly, we explore the effects of the Bond
surface albedo on the polarization and albedo phase curves. The surface
features of such planets are known to significantly dictate the nature of
these observational quantities. We also determine the effect of the inclination
angle and the clouds for two different wavebands i.e. visible and
infrared. Our findings indicate that the clouds serve as an indicator for the
polarization due to scattering for the terrestrial exoplanets.
More information can be extracted through the synergistic observations of spectra and phase curves. Additionally, the degeneracy among the estimated
parameters of terrestrial exoplanets can be reduced by characterizing
the atmospheres through various methods like, reflection spectra, transmission
spectra and polarization phase curves. Consequently, our models will
be instrumental in guiding future observations and enhancing the precision
of exoplanetary atmospheric characterization.