JpGU-AGU Joint Meeting 2017

Presentation information

[EE] Oral

A (Atmospheric and Hydrospheric Sciences) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS01] [EE] 3D Cloud Modeling as a Tool for 3D Radiative Transfer, and Conversely

Sun. May 21, 2017 10:45 AM - 12:15 PM 304 (International Conference Hall 3F)

convener:Thomas Fauchez(Universities Space Research Association, GSFC Greenbelt), Anthony B Davis(Jet Propulsion Laboratory), Hironobu Iwabuchi(Graduate School of Science, Tohoku University), Kentaroh Suzuki(Atmosphere and Ocean Research Institute, University of Tokyo), Chairperson:Thomas Fauchez(Universities Space Research Association, GSFC Greenbelt)

11:40 AM - 12:00 PM

[AAS01-09] Using polarimetry to retrieve the cloud coverage of Earth-like exoplanets

★Invited papers

*Loic Rossi1, Daphne M Stam1 (1.Faculty of Aerospace Engineering, Delft University of Technology)

Keywords:polarimetry, atmospheres, exoplanets, clouds

Clouds in atmospheres of exoplanets play a key role in understanding their climate and radiative balance. They can also complicate the detection of chemical species in the atmosphere by flattening the spectra or by creating degeneracies between observables (Kitzmann et al. 2011, Line and Parmentier 2016)

Polarimetry promises to be a powerfull tool to detect and study exoplanets (Stam et al. 2004). The polarisation of the light scattered by the atmosphere of those planets contains a lot of information about the vertical structure of the atmosphere and about the composition of the clouds (Karalidi et al. 2012) and has already been very successful in the case of Venus (Rossi et al. 2015, 2016 in prep).

We used radiative transfer models based on the doubling-adding method to simulate the disk-integrated flux and polarization of light scattered by exoplanets with patchy, subsolar and polar water clouds. We show that the degree of polarization of the light scattered by an exoplanet can be used to discriminate between the different types of cloud coverage and to quantify the cloud coverage on the planetary scale. Use of both flux and polarization allows for a resolution of some ambiguities between cloud coverage and cloud top altitudes.

We then propose an observational strategy based on an iterative process using polarization phase curves in the wavelength range 300 to 900 nm that could help retrieve both orbital parameters and cloud coverage with minor ambiguities.

We intend to test this method using GCM outputs to simulate the cloud cover and the resulting flux and polarization of some exoplanets.