User:Ceholloway45/Atmospheric Escape of Exoplanet Atmospheres
References
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As of April 2026, there are 6,160 confirmed exoplanets, with over 7,000 yet-to-be confirmed [nasa exoplanet archive]. By combining various methods, such as the transiting and radial velocity, it is possible to derive estimates for these planets. The bulk of |
As of April 2026, there are 6,160 confirmed exoplanets, with over 7,000 yet-to-be confirmed [nasa exoplanet archive]. By combining various methods, such as the transiting and radial velocity, it is possible to derive estimates for these planets. The bulk of these planets are Super-Earths and sub-Neptunes, types with no Solar System analogs [1]. Additionally, there are few planets, with radii between 1.3 - 2.5 $R_{\Earth}$, between these types. This gap is known as the "radius valley." Recently, it has been proposed that terrestrial planets could obtain their size through atmospheric escape [3]. |
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Atmospheres are hypothesized to be a collection of atoms and molecules that exist in a quasi-hydrostatic state. When incident short-wave radiation heats the thermosphere, the upper thermosphere becomes isothermic through conduction. The upper thermosphere is separated by the exobase-level. This is the boundary that separates the collision-dominated and collision-less regions. At certain temperatures above the exobase, collision-less region, light atmospheric species can become energetic enough to escape the gravitational potential of the planet, escaping into space [Lammer 2013]. This process is known as the jeans escape. This process can only occur within the collision-less region. The region below the exobase, a collision-dominated region, is in hydrostatic equilibrium. However, in conditions of intense extreme Ultraviolet and X-rays, the bulk gasses within the collision-less region can become energetic enough to cause hydrodynamic outflows, similar to Parker winds (Hazra 2025). Atmospheric escape can occur in two categories: non-thermal and thermal. The two processes mentioned earlier, Hydrodynamic and Jean escape, are two major thermal atmospheric escape mechanisms that may be responsible for the "radius valley" gap. |
Atmospheres are hypothesized to be a collection of atoms and molecules that exist in a quasi-hydrostatic state. When incident short-wave radiation heats the thermosphere, the upper thermosphere becomes isothermic through conduction. The upper thermosphere is separated by the exobase-level. This is the boundary that separates the collision-dominated and collision-less regions. At certain temperatures above the exobase, collision-less region, light atmospheric species can become energetic enough to escape the gravitational potential of the planet, escaping into space [Lammer 2013]. This process is known as the jeans escape. This process can only occur within the collision-less region. The region below the exobase, a collision-dominated region, is in hydrostatic equilibrium. However, in conditions of intense extreme Ultraviolet and X-rays, the bulk gasses within the collision-less region can become energetic enough to cause hydrodynamic outflows, similar to Parker winds (Hazra 2025). Atmospheric escape can occur in two categories: non-thermal and thermal. The two processes mentioned earlier, Hydrodynamic and Jean escape, are two major thermal atmospheric escape mechanisms that may be responsible for the "radius valley" gap. |
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=== References === |
=== References === |
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# '''Seager, Sara; Deming, Drake (2010). “Exoplanet Atmospheres.” ''Annual Review of Astronomy and Astrophysics'', 48: 631–672. doi:10.1146/annurev-astro-081309-130837. |
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'''(exoplanetarchive.ipac.caltech.edu in Bing)''' |
# '''NASA Exoplanet Science Institute (2024). ''NASA Exoplanet Archive''. California Institute of Technology. Retrieved 20 April 2026, from''' '''(exoplanetarchive.ipac.caltech.edu in Bing)''' |
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# '''Fulton, Benjamin J.; Petigura, Erik A.; Howard, Andrew W.; Isaacson, Howard; Marcy, Geoffrey W.; Cargile, Phillip A.; Hebb, Leslie; Weiss, Lauren M.; Johnson, John Asher; Morton, Timothy D.; Sinukoff, Evan; Crossfield, Ian J. M.; Hirsch, Lea A. (2017). “The California‑Kepler Survey. III. A Gap in the Radius Distribution of Small Planets.” ''The Astronomical Journal'', 154 (3): 109. doi:10.3847/1538‑3881/aa80eb.''' |
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# '''Perryman, Michael (2018). ''The Exoplanet Handbook'' (2nd ed.). Cambridge University Press. ISBN 978‑1‑108‑42234‑3.''' |
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# '''Lammer, Helmut (2013). ''Origin and Evolution of Planetary Atmospheres: Implications for Habitability''. Springer. ISBN 978‑3‑642‑32086‑6.''' |
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# '''Hazra, Gopal (2025). “Atmospheric Escape Processes of Exoplanets.” ''Annual Review of Earth and Planetary Sciences'', 53: 1–34. doi:10.1146/annurev-earth-090124‑015432.''' |
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