University Adina Feinstein, Sagan Fellow University of Colorado Boulder Probing the atmospheric composition of young planets Informing planet formation & evolution 1 July 5, 2024 EAS SS13
& ice core • Planets form at or beyond the water ice line, where accretion rates are accelerated. • Planets migrate in after formation to their current-day locations. • Planetary atmospheres would be volatile & water enriched. Morbidelli et al. (2015); Johansen et al. (2017); Batygin & Morbidelli (2023)
Rock core • Planets form within the water ice line • Pebbles which migrated inwards are partially or fully devolatalized. • Planetary atmosphere would be primarily H & He and volatile depleted. Boley, Morris, & Ford (2014); Chatterjee & Tan (2014, 2015); Batygin & Morbidelli (2023)
different levels of instellation. 19 (Barat et al. 2024; Barat et al. submitted) Saugata Barat University of Amsterdam SPlanet b = 35 S⨁ SPlanet c = 146 S⨁
reveals a huge CO2 and no significant SO2 feature. 23 Pa Chia Thao University of North Carolina Chapel Hill (Thao, Mann, Feinstein et al. under review) H2O CO2 SO2
NIR/ IR observations of young planetary atmospheres. 34 JWST GO 5311, 5959 - Co-PIs Feinstein & Welbanks JWST GO 5882 - Co-PIs Dai & Petigura V1298 Tau cde TOI 451 cd TOI 2076 bcd 120 205 23 System Age [Myr] Orbital Separation [AU] 0 0.08 0.3 0.1 22 AU Mic b 0.2
[email protected] -How does atmospheric metallicity evolve? -When do young planets transition from cloudless to cloudy? -Where are all the primordial hot Jupiters? -What do all of these new pieces of information tell us about the diversity of planet formation, both in the same system and between systems? ADS Library for young planet atmospheric characterization publications