# Dusty outflows in planetary atmospheres: Understanding "super-puffs" and   transmission spectra of sub-Neptunes

**Authors:** Lile Wang, Fei Dai

arXiv: 1902.04188 · 2019-03-06

## TL;DR

This paper proposes that dusty, non-static atmospheric outflows in super-puff exoplanets explain their large apparent radii and flat transmission spectra, challenging static atmospheric models and impacting exoplanet characterization.

## Contribution

It introduces a novel scenario of dusty outflows carrying small dust grains to high altitudes, explaining observations of super-puffs and their flat spectra, which static models cannot.

## Key findings

- Dusty outflows can inflate transit radii.
- High-altitude dust flattens transmission spectra.
- Scenario explains super-puff observations.

## Abstract

`Super-puffs' are planets with anomalously low mean densities ($\lesssim 10^{-1}~{\rm g\ cm}^{-3}$). With a low surface gravity, the extended atmosphere is susceptible to extreme hydrodynamic mass loss (`boil off') on a timescale much shorter than the system's age. Even more puzzling, super-puffs are estimated to have a scale height of $\sim 3000~{\rm km}$, yet recent observations revealed completely flat transmission spectra for Kepler 51b and 51d. We investigate a new scenario that explains both observations: non-static outflowing ($\dot{M}\gtrsim 10^{-10}~M_\oplus~{\rm yr}^{-1}$) atmospheres that carry very small dust grains ($\sim 10~{\rm A}$ in size, $\sim 10^{-2}$ in mass fraction) to high altitudes ($\lesssim 10^{-6}~{\rm bar}$). Dust at high altitudes inflates the observed transit radius of the planet while flattens the transmission spectra.Previous static atmospheric models struggles to achieve cloud elevation and production of photochemical haze at such high altitudes. We propose to test this scenario by extending the wavelength coverage of transmission spectra. If true, dusty atmospheric outflows may affect many young ($\lesssim 10^9~{\rm yr}$), low mass ($\lesssim 10~M_\oplus$) exoplanets, thereby limit our ability to study the atmospheric composition in transmission, and inflate the observed transit radius of a planet hence obscure the underlying mass-radius relationship.

## Full text

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## Figures

6 figures with captions in the complete paper: https://tomesphere.com/paper/1902.04188/full.md

## References

35 references — full list in the complete paper: https://tomesphere.com/paper/1902.04188/full.md

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Source: https://tomesphere.com/paper/1902.04188