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Characterizing Earth-like Exoplanets: Insights from Earthshine Observations

Giulia, Roccetti

Abstract

The next generation of ground- and space-based telescopes, such as ANDES and PCS at the ELT and the mission concept Habitable World Observatory (HWO), will enable the study of exoplanets in reflected light, extending this capability to rocky planets. To better understand Earth as an exoplanet, we analyze its spatially unresolved visible reflected spectrum via the sunlight reflected by Earth onto the Moon (Earthshine). Using the 3D Monte Carlo radiative transfer code MYSTIC, we generate synthetic spectra and phase curves of Earth in both intensity and polarization, incorporating realistic 3D atmospheric pressure-temperature profiles, patchy clouds, and wavelength-dependent surface albedo maps. By comparing these simulations with Earthshine data, we evaluate the sensitivity of key spectral features for planetary characterization and habitability assessment. Our findings highlight the necessity of detailed atmospheric and surface albedo modeling to accurately reproduce Earthshine observations. These insights are essential for future missions targeting Earth-like exoplanet characterization. By advancing our understanding of Earth's radiative and spectral properties, we establish a basis for interpreting observations of similar distant planets. We also formulate an optimal strategy, through a comparison of spectroscopy and spectropolarimetry, for assessing the chemical diversity of Earth-like exoplanets with upcoming telescopes.

Full text

Characterizing Earth-like Exoplanets: Insights from Earthshine Observations G I U L I A R O C C E T T I - E S O & L M U w i t h MI C H AE L S T ER ZI K ( ESO ) CL AU DI A E MDE ( LM U ) MI H AI L MA N EV ( LM U ) JU L IA S E I DEL (E SO ) ST EF A NO BA GN U LO ( ARM AG H) E A R T H S H I N E O B S E R V A T I O N S •Sunlight scattered by Earth’s atmosphere and reflected from the lunar surface •The Moon acts as a diffuse mirror •Resemble reflected light observations of exoplanets H O W TO S T U D Y T H E E A R T H AS AN E X O P L A N E T S A T E L L I T E O B S E R V A T I O N S E X O P L A N E T S O B S E R V A T I O N S •high spatial resolution •local properties •low spectral resolution •spatially unresolved •disk-integrated properties •high spectral resolution E A R T H S H I N E IN P O L A R I S A T I O N •Polarisation : no need to correct for the transmission through Earth’s atmosphere •Enhance the contrast between the planet and the star •More information on the properties of the planet SURFACE REFLECTION OCEAN GLINTCLOUD DROPLETS W H A T C A U S E S P O L A R I S A T I O N ? SINGLE SCATTERING MOLECULES DEPOLARISATION CLOUDS AND AEROSOLS Ocean C A T A L O G U E OF T H E O B S E R V A T I O N S Ocean Ocean Ocean OceanRocky Rocky Rocky Roccetti+ 2025c (in prep.) M O D E L L I N G E A R T H S H I N E MYSTIC – Monte Carlo code for phYsically correct Tracing of photons in Cloudy atmospheres •Realistic 3D atmospheres •Inhomogeneous clouds and surfaces Mayer&Kylling 2005 Emde+ 2016 M O D E L L I N G E A R T H S H I N E •Emde+ 2017 showed the importance of the ocean glint feature •Simulations could not fit the observations in polarisation •Simplistic assumptions on clouds and planetary surfaces Emde+ 2017 P L A N E T A R Y S U R F A C E Hyperspectral Albedo Maps dataset with high Spatial and TEmporal Resolution (HAMSTER) •PCA regression algorithm •Interpolate MODIS albedo product among its 7 bands in the VIS/NIR Hyperspectral nature of surface reflectivity is key Roccetti+ 2024 S U R F A C E V A R I A B I L I T Y : O C E A N VS. L A N D Roccetti+ 2025c (in prep.) T A K E H O M E M E S S A G E S •Earthshine allows to characterise Earth as a spatially unresolved exoplanet at different phase angles •Reflected light simulations are very sensitive to clouds and planetary surfaces •Polarisation can distinguish ocean vs. land surfaces •VRE is overestimated if not considering linear combination of different surface types Giulia Roccetti - [email protected]