JWSTデータでハビタブルゾーンに驚くべき氷の世界を発見(Astronomers find surprising ice world in the habitable zone with JWST data)

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2024-07-08 ミシガン大学

ミシガン大学の天文学者を含むチームは、居住可能なスーパーアースとして有望な温帯の太陽系外惑星LHS 1140 bを特定しました。約48光年離れたクジラ座に位置するこの惑星は、厚い水素リッチな大気を持つミニ・ネプチューンではなく、氷や水に富む可能性があります。研究者たちは、ジェームズ・ウェッブ宇宙望遠鏡などのデータを用いてこの惑星が窒素リッチな大気を持つスーパーアースである可能性を示しました。LHS 1140 bは液体の水を持つ可能性があり、将来の居住可能性研究において重要な対象となります。

<関連情報>

JWST/NIRISSによるハビタブルゾーン太陽系外惑星LHS 1140 bの透過分光観測 Transmission Spectroscopy of the Habitable Zone Exoplanet LHS 1140 b with JWST/NIRISS

Charles Cadieux, René Doyon, Ryan J. MacDonald, Martin Turbet, Étienne Artigau, Olivia Lim, Michael Radica, Thomas J. Fauchez, Salma Salhi, Lisa Dang, Loïc Albert, Louis-Philippe Coulombe, Nicolas B. Cowan, David Lafrenière, Alexandrine L’Heureux, Caroline Piaulet, Björn Benneke, Ryan Cloutier, Benjamin Charnay, Neil J. Cook, Marylou Fournier-Tondreau, Mykhaylo Plotnykov, Diana Valencia
arXiv  Submitted on 21 Jun 2024
DOI:https://doi.org/10.48550/arXiv.2406.15136

JWSTデータでハビタブルゾーンに驚くべき氷の世界を発見(Astronomers find surprising ice world in the habitable zone with JWST data)

Abstract

LHS 1140 b is the second-closest temperate transiting planet to the Earth with an equilibrium temperature low enough to support surface liquid water. At 1.730±0.025 R⊕, LHS 1140 b falls within the radius valley separating H2-rich mini-Neptunes from rocky super-Earths. Recent mass and radius revisions indicate a bulk density significantly lower than expected for an Earth-like rocky interior, suggesting that LHS 1140 b could either be a mini-Neptune with a small envelope of hydrogen (∼0.1% by mass) or a water world (9–19% water by mass). Atmospheric characterization through transmission spectroscopy can readily discern between these two scenarios. Here, we present two JWST/NIRISS transit observations of LHS 1140 b, one of which captures a serendipitous transit of LHS 1140 c. The combined transmission spectrum of LHS 1140 b shows a telltale spectral signature of unocculted faculae (5.8 σ), covering ∼20% of the visible stellar surface. Besides faculae, our spectral retrieval analysis reveals tentative evidence of residual spectral features, best-fit by Rayleigh scattering from an N2-dominated atmosphere (2.3 σ), irrespective of the consideration of atmospheric hazes. We also show through Global Climate Models (GCM) that H2-rich atmospheres of various compositions (100×, 300×, 1000×solar metallicity) are ruled out to >10 σ. The GCM calculations predict that water clouds form below the transit photosphere, limiting their impact on transmission data. Our observations suggest that LHS 1140 b is either airless or, more likely, surrounded by an atmosphere with a high mean molecular weight. Our tentative evidence of an N2-rich atmosphere provides strong motivation for future transmission spectroscopy observations of LHS 1140 b.

1701物理及び化学
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