太陽系外惑星Trappist-1 bには大気があるのか?(Does the exoplanet Trappist-1 b have an atmosphere after all?)

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2024-12-16 マックス・プランク研究所

マックス・プランク研究所の研究者たちは、ジェームズ・ウェッブ宇宙望遠鏡(JWST)を用いて、地球サイズの岩石惑星TRAPPIST-1 bの観測を行いました。これまで、この惑星は大気を持たないと考えられていましたが、最新の観測結果はその可能性を再評価する必要があることを示唆しています。観測データによれば、TRAPPIST-1 bの表面には風化の兆候が見られず、これは火山活動やプレートテクトニクスなどの地質活動が存在する可能性を示しています。一方で、二酸化炭素からなる薄い大気が存在する可能性も否定できません。これらの結果は、薄い大気を持つエクソプラネットの特性を特定することの難しさを浮き彫りにしています。

<関連情報>

12.8μmと15μmのJWST/MIRIによるTRAPPIST-1 bの食観測の複合解析 Combined analysis of the 12.8 and 15 μm JWST/MIRI eclipse observations of TRAPPIST-1 b

Elsa Ducrot,Pierre-Olivier Lagage,Michiel Min,Michaël Gillon,Taylor J. Bell,Pascal Tremblin,Thomas Greene,Achrène Dyrek,Jeroen Bouwman,Rens Waters,Manuel Güdel,Thomas Henning,Bart Vandenbussche,Olivier Absil,David Barrado,Anthony Boccaletti,Alain Coulais,Leen Decin,Billy Edwards,René Gastaud,Alistair Glasse,Sarah Kendrew,Goran Olofsson,Polychronis Patapis,… Gillian Wright
Nature astronomy  Published:16 December 2024
DOI:https://doi.org/10.1038/s41550-024-02428-z

太陽系外惑星Trappist-1 bには大気があるのか?(Does the exoplanet Trappist-1 b have an atmosphere after all?)

Abstract

The first James Webb Space Telescope/MIRI photometric observations of TRAPPIST-1 b allowed for the detection of the thermal emission of the planet at 15 μm, suggesting that the planet could be a bare rock with a zero albedo and no redistribution of heat. These observations at 15 μm were acquired as part of Guaranteed Time Observer time that included a twin programme at 12.8 μm to obtain measurements inside and outside the CO2 absorption band. Here we present five new occultations of TRAPPIST-1 b observed with MIRI in an additional photometric band at 12.8 μm. We perform a global fit of the ten eclipses and derive a planet-to-star flux ratio and 1σ error of 452 ± 86 ppm and 775 ± 90 ppm at 12.8 μm and 15 μm, respectively. We find that two main scenarios emerge. An airless planet model with an unweathered (fresh) ultramafic surface, that could be indicative of relatively recent geological processes, fits the data well. Alternatively, a thick, pure-CO2 atmosphere with photochemical hazes that create a temperature inversion and result in the CO2 feature being seen in emission also works, although with some caveats. Our results highlight the challenges in accurately determining a planet’s atmospheric or surface nature solely from broadband filter measurements of its emission, but also point towards two very interesting scenarios that will be further investigated with the forthcoming phase curve of TRAPPIST-1 b.

1701物理及び化学
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