典型热木星 HD 189733 b 日侧大气中的石英云

Julie Inglis, Natasha E. Batalha, Nikole K. Lewis, Tiffany Kataria, Heather A. Knutson, Brian M. Kilpatrick, Anna Gagnebin, Sagnick Mukherjee, Maria M. Pettyjohn, Ian J. M. Crossfield, Trevor O. Foote, David Grant, Gregory W. Henry, Maura Lally, Laura K. McKemmish, David K. Sing, Hannah R. Wakeford, Juan C. Zapata Trujillo and Robert T. Zellem
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摘要

最近利用JWST的中红外低分辨光谱仪(MIRI LRS)进行的中红外观测首次在两颗凌日系外行星WASP-17 b和WASP-107 b的透射光谱中直接探测到了硅酸盐云的吸收特征。我们证实了之前从斯皮策红外摄谱仪(IRS)上探测到的 6.5 μm 处的 H2O 吸收,并在两次二次日食观测中探测到了 H2S 以及 8.7 μm 处的吸收特征。8.7 μm处的过量吸收可以解释为HD 189733 b日侧大气最上层存在小的(∼0.01 μm)SiO2[s]颗粒。这是首次直接探测到HD 189733 b大气中的硅酸盐云,也是首次探测到任何热木星日侧硅酸盐云的明显吸收特征。我们发现,包含二氧化硅[s]的模型比透明模型和包含其他潜在云种类的模型更优越6-7σ。这些硅酸盐粒子的高空位置最好解释为是在HD 189733 b靠近亚恒星点的日侧大气最热区域形成的。我们还发现,HD 189733 b 在 9 μm 以远的发射光谱显示了一些残余特征,而我们目前的大气模型并不能很好地捕捉到这些特征。结合 JWST 在较短波长上对 HD 189733 b 的透射和发射光谱进行的其他观测,这些观测将为我们提供迄今为止关于这颗基准热木星的大气成分和云层特性的最详细描述。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Quartz Clouds in the Dayside Atmosphere of the Quintessential Hot Jupiter HD 189733 b
Recent mid-infrared observations with JWST's Mid-Infrared Instrument Low Resolution Spectrometer (MIRI LRS) have resulted in the first direct detections of absorption features from silicate clouds in the transmission spectra of two transiting exoplanets, WASP-17 b and WASP-107 b. In this Letter, we measure the mid-infrared (5–12 μm) dayside emission spectrum of the benchmark hot Jupiter HD 189733 b with MIRI LRS by combining data from two secondary-eclipse observations. We confirm the previous detection of H2O absorption at 6.5 μm from Spitzer's Infrared Spectrograph (IRS) and additionally detect H2S as well as an absorption feature at 8.7 μm in both secondary-eclipse observations. The excess absorption at 8.7 μm can be explained by the presence of small (∼0.01 μm) grains of SiO2[s] in the uppermost layers of HD 189733 b’s dayside atmosphere. This is the first direct detection of silicate clouds in HD 189733 b’s atmosphere, and the first detection of a distinct absorption feature from silicate clouds on the dayside of any hot Jupiter. We find that models including SiO2[s] are preferred by 6–7σ over clear models and those with other potential cloud species. The high-altitude location of these silicate particles is best explained by formation in the hottest regions of HD 189733 b’s dayside atmosphere near the substellar point. We additionally find that HD 189733 b’s emission spectrum longward of 9 μm displays residual features not well captured by our current atmospheric models. When combined with other JWST observations of HD 189733 b’s transmission and emission spectra at shorter wavelengths, these observations will provide us with the most detailed picture to date of the atmospheric composition and cloud properties of this benchmark hot Jupiter.
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