Habitable Zone and Atmosphere Retention Distance (HaZARD) Stellar-evolution-dependent loss models of secondary atmospheres
arXiv:2502.09702 · doi:10.1051/0004-6361/202452998
Abstract
A major open question in exoplanet research is whether secondary atmospheres are rare around Earth-sized rocky exoplanets. In this work we determine the distance at which an Earth-sized planet orbiting a variety of stellar hosts could retain a CO2- or N2-dominated atmosphere and compare this atmospheric retention distance (ARD) with that of the liquid-water HZ. We combined planetary atmosphere models with stellar evolution models. The atmospheric models produced by the thermochemical Kompot code allowed us to calculate the Jeans escape rates for different stellar masses, rotation rates, and ages. These loss rates allowed us to determine the closest distance a planet is likely to retain a CO2- or N2-dominated atmosphere. Using stellar rotation evolution models, we modelled how these retention distances evolve as the X-ray and ultraviolet activity of the star evolves. We find that the overlap of the HZ and the ARD occurs earlier around slowly rotating stars. Additionally, we find that HZ planets orbiting stars with masses under 0.4 M_\odot are unlikely to retain any atmosphere, due to the lower spin-down rate of these fully convective stars. We also show that the initial rotation rate of the star can impact the likelihood of a planet retaining an atmosphere, as an initially fast-rotating star maintains high levels of short-wavelength irradiance for much longer. The orbits of all Earth-like rocky exoplanets observed by JWST in cycles 1 and 2, including HZ planets, fall outside the ARD. Our results will have implications for future target selections of small exoplanet observing programmes with JWST or future instruments such as the Ariel space mission.
10 pages, 5 figures, accepted for publication in A&A
References in corpus (21)
- The James Webb Space Telescope
- Seven temperate terrestrial planets around the nearby ultracool dwarf star TRAPPIST-1
- Most 1.6 Earth-Radius Planets are not Rocky
- Habitable Zones Around Main-Sequence Stars: Dependence on Planetary Mass
- The faint young Sun problem
- The Extreme Ultraviolet and X-Ray Sun in Time: High-Energy Evolutionary Tracks of a Solar-Like Star
- Observing the Atmospheres of Known Temperate Earth-sized Planets with JWST
- Thermal emission from the Earth-sized exoplanet TRAPPIST-1 b using JWST
- The Detectability and Characterization of the TRAPPIST-1 Exoplanet Atmospheres with JWST
- Nitrogen Isotopic Composition and Density of the Archean Atmosphere
- The Habitable Zones of Pre-Main-Sequence Stars
- Magma oceans and enhanced volcanism on TRAPPIST-1 planets due to induction heating
- Modeling pN2 through Geological Time: Implications for Planetary Climates and Atmospheric Biosignatures
- Hubble WFC3 Spectroscopy of the Habitable-zone Super-Earth LHS 1140 b
- The Role of N2 as a Geo-Biosignature for the Detection and Characterization of Earth-like Habitats
- Hydrodynamic escape of water vapor atmospheres near very active stars
- Survival of Terrestrial N2-O2 Atmospheres in Violent XUV Environments through Efficient Atomic Line Radiative Cooling
- The young Sun's XUV-activity as a constraint for lower CO-limits in the Earth's Archean atmosphere
- Airy worlds or barren rocks? On the survivability of secondary atmospheres around the TRAPPIST-1 planets
- Low volcanic outgassing rates for a stagnant lid Archean Earth with graphite-saturated magmas
- Reconstructing the XUV Spectra of Active Sun-like Stars Using Solar Scaling Relations with Magnetic Flux