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, Robert T. Zellem
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引用次数: 0

摘要

最近利用JWST/MIRI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的发射光谱中直接探测到了硅酸盐云的吸收特征。在本文中,我们利用MIRI LRS测量了基准热木星HD 189733 b的中红外(5-12 $\mu$m)日侧发射光谱,并结合了两次日食观测的数据。我们证实了之前 Spitzer/IRS 在 6.5 波长处探测到的 H$_2$O 吸收,并且在两次日食观测中都探测到了 H$_2$S 以及 8.7 波长处的吸收特征。8.7波长处的过量吸收可以用HD 189733 b日侧大气最上层存在的SiO$_2$[s]小颗粒(0.01波长)来解释。这是首次直接探测到HD 189733 b大气中的硅酸盐云,也是首次探测到热木星日侧硅酸盐云的明显吸收特征。我们发现,包含 SiO$_2$[s] 的模型比清澈模型和包含其他潜在云物种的模型更受青睐,相差 6-7 美元。这些硅酸盐粒子的高空位置,最好的解释是在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的发射光谱在波长9$\mu$m处显示出残余特征,而我们目前的大气模型并不能很好地捕捉到这些特征。如果与 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结合起来,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构成和云特性的最详尽图像。
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/MIRI 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 paper, we measure the mid-infrared ($5-12$ $\mu$m) 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 H$_2$O absorption at 6.5 $\mu$m from Spitzer/IRS and additionally detect H$_2$S as well as an absorption feature at 8.7 $\mu$m in both secondary eclipse observations. The excess absorption at 8.7 $\mu$m can be explained by the presence of small ($\sim$0.01 $\mu$m) grains of SiO$_2$[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 day side of any hot Jupiter. We find that models including SiO$_2$[s] are preferred by $6-7\sigma$ 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 $\mu$m 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 spectrum 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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