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arXiv 2406.09641astro-ph.EP
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利用GEMINI-S/IGRINS解析超热木星WASP-121b大气中水和一氧化碳的吸收特征随轨道相位的变化

Phase-resolving the absorption signatures of water and carbon monoxide in the atmosphere of the ultra-hot Jupiter WASP-121b with GEMINI-S/IGRINS

Joost P. Wardenier, Vivien Parmentier, Michael R. Line, Megan Weiner Mansfield, Xianyu Tan, Shang-Min Tsai, Jacob L. Bean, Jayne L. Birkby, Matteo Brogi, Jean-M… 展开作者

Joost P. Wardenier, Vivien Parmentier, Michael R. Line, Megan Weiner Mansfield, Xianyu Tan, Shang-Min Tsai, Jacob L. Bean, Jayne L. Birkby, Matteo Brogi, Jean-Michel Désert, Siddharth Gandhi, Elspeth K. H. Lee, Colette I. Levens, Lorenzo Pino, Peter C. B. Smith

AI总结:

利用Gemini-S/IGRINS对超热木星WASP-121b进行三次凌星观测,首次测量CO和H₂O的相位相关吸收信号,发现二者空间分布不同,并揭示大气拖曳效应,凸显相位分辨光谱对研究超热木星大气三维结构的重要性。

摘要:

超热木星是高光谱分辨率大气表征的最佳目标之一。解析其透射光谱随轨道相位的变化,为揭示这些天体的三维性质提供了独特的窗口。在本工作中,我们展示了利用Gemini-S/IGRINS观测到的超热木星WASP-121b的三次凌星数据。我们首次测量了系外行星大气中CO和H$_2$O的相位相关吸收信号,并发现它们存在差异。在凌星过程中,CO的蓝移逐渐增大,而H$_2$O的吸收线随相位变化蓝移逐渐减小,甚至在凌星后半段出现红移。这些测量揭示了这两种分子在超热木星大气中不同的空间分布。此外,我们发现H$_2$O信号在凌星的前四分之一阶段缺失,这可能暗示WASP-121b的黄昏终结者附近存在云的形成。为了进一步解释CO和H$_2$O的吸收轨迹,以及先前利用VLT/ESPRESSO测得的Fe的多普勒位移,我们将数据与WASP-121b的模拟凌星进行了比较。为此,我们使用三维蒙特卡洛辐射传输代码对全球环流模型的输出进行了后处理。我们的分析表明,WASP-121b的大气受到大气拖曳的影响,这与先前根据相位曲线观测推断出的小热斑偏移一致。我们的研究强调了相位分辨光谱在揭示超热木星复杂大气结构中的重要性,并为其化学和动力学特性的进一步研究奠定了基础。

英文摘要:

Ultra-hot Jupiters are among the best targets for atmospheric characterization at high spectral resolution. Resolving their transmission spectra as a function of orbital phase offers a unique window into the 3D nature of these objects. In this work, we present three transits of the ultra-hot Jupiter WASP-121b observed with Gemini-S/IGRINS. For the first time, we measure the phase-dependent absorption signals of CO and H$_{\text{2}}$O in the atmosphere of an exoplanet, and we find that they are different. While the blueshift of CO increases during the transit, the absorption lines of H$_{\text{2}}$O become less blueshifted with phase, and even show a redshift in the second half of the transit. These measurements reveal the distinct spatial distributions of both molecules across the atmospheres of ultra-hot Jupiters. Also, we find that the H$_{\text{2}}$O signal is absent in the first quarter of the transit, potentially hinting at cloud formation on the evening terminator of WASP-121b. To further interpret the absorption trails of CO and H$_{\text{2}}$O, as well as the Doppler shifts of Fe previously measured with VLT/ESPRESSO, we compare the data to simulated transits of WASP-121b. To this end, we post-processes the outputs of global circulation models with a 3D Monte-Carlo radiative transfer code. Our analysis shows that the atmosphere of WASP-121b is subject to atmospheric drag, as previously suggested by small hotspot offsets inferred from phase-curve observations. Our study highlights the importance of phase-resolved spectroscopy in unravelling the complex atmospheric structure of ultra-hot Jupiters and sets the stage for further investigations into their chemistry and dynamics.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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