Using the helium triplet as a tracer of the physics of giant planet outflows
Matth\"aus Schulik, James Owen

TL;DR
This paper uses radiation-hydrodynamic simulations to study helium triplet emissions as tracers of giant planet outflows, revealing insights into their cooling, ionization, and observational signatures.
Contribution
It introduces a novel application of helium triplet observations to understand the physics of giant planet atmospheric outflows, including adiabatic cooling and fractionation effects.
Findings
Helium triplet excess explains observed spectral broadening in HD 189733b.
Adiabatic cooling confirms hydrodynamic outflow nature on several planetary radii.
Helium triplet is less prone to fractionation than ground-state helium, affecting transit depth predictions.
Abstract
Hydrodynamic outflows, such as those observed escaping close-in gas giant planets, are not isothermal in structure. Their highly ionized nature allows them to cool adiabatically at distances beyond several planetary radii. The contrast between the hottest gas temperatures at around 10,000K and the coldest at around 1,000K triggers an excess population of the observable helium triplet. This excess is caused by the suppression of collisional de-excitation from the triplet state at cool temperatures. Using radiation-hydrodynamic simulations, we show that this helium triplet excess may explain the excess broadening seen in HD 189733b's observed transmission spectrum, demonstrating adiabatic cooling of its outflow, confirming its hydrodynamic nature on scales of several planetary radii. However, further observations are required to confirm this conclusion. Furthermore, we explore a range of…
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Taxonomy
TopicsAstro and Planetary Science · Spacecraft and Cryogenic Technologies · Geomagnetism and Paleomagnetism Studies
