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Atmospheric Retrieval of Cloudy Venus-Twin Exoplanets in the Context of the LIFE Mission
(2021)EPSC AbstractsOther Conference Item -
Diagnostic potential of the mid-infrared space interferometer LIFE for studying Earth analogues
(2021)EPSC AbstractsOther Conference Item -
The Large Interferometer For Exoplanets (LIFE) mission: status and progress report
(2021)EPSC AbstractsOther Conference Item -
LIFEsim: Methods for predicting the capability of the future LIFE mission
(2021)EPSC AbstractsOther Conference Item -
Exoplanet yield predictions for the future LIFE mission
(2021)EPSC AbstractsOther Conference Item -
On the importance of including devolatilized stellar abundances in determining the composition of rocky exoplanets
(2021)EGUsphereSince stars and their planets form from the same molecular clouds, stellar chemical composition can be informative, to first order, of planetary bulk chemistry. An important feature of terrestrial planets compared to their host stars is the depletion of volatiles, the most important being oxygen. Previous studies on planet interiors focus on the mass and radius constraints and/or the host stellar refractory elements (e.g. Fe, Si and Mg), ...Other Conference Item -
The LIFE mission: a mid-infrared space interferometer to study the diversity of terrestrial exoplanets
(2020)EPSC AbstractsOther Conference Item -
LIFEsim: Methods for predicting the exoplanet yield of the future LIFE mission
(2022)Bulletin of the American Astronomical Society ~ AASTCS 9: Exoplanets IV AbstractsOther Conference Item -
The Large Interferometer for Exoplanets (LIFE): probing the diversity of terrestrial exoplanet atmospheres in the mid-infrared
(2022)Bulletin of the American Astronomical Society ~ AASTCS 9: Exoplanets IV AbstractsOther Conference Item -
No universal devolatilization trend has been found for the solar system rocky bodies
(2022)EPSC AbstractsRocky planets formed at different heliocentric distances from the Sun are thought to experience different and systematic devolatilization (i.e. depletion of volatile elements) with respect to the solar composition. The canonical empirical model of devolatilization is calibrated based on the bulk compositional difference between the Sun and Earth as a function of 50% condensation temperature of elements (TC). The quantification of the ...Other Conference Item