可爱揭示了超热木星WASP-189b上层大气中逃逸的金属

A. Sreejith, K. France, L. Fossati, T. Koskinen, A. Egan, P. Cauley, P. Cubillos, S. Ambily, Chenliang Huang, P. Lavvas, B. Fleming, J. Désert, N. Nell, P. Petit, A. Vidotto
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摘要

对温度超过2000 K的超热木星(系外行星)的紫外线观测为我们提供了一个研究大气逃逸是否以及如何塑造其上层大气的机会。近紫外传输光谱为研究这一过程提供了一个独特的工具,因为存在强金属谱线和明亮的光球连续体作为观察吸收气体的光源。WASP-189b是迄今为止发现的最热的行星之一,它的白天温度约为3400 K,围绕一颗明亮的a型恒星运行。我们提出了第一次对WASP-189b的近紫外观测,这是由科罗拉多紫外过境实验(CUTE)获得的。CUTE是美国宇航局资助的一项6U紫外光谱任务,致力于监测短周期凌日行星。WASP-189b是CUTE早期的科学目标之一,在2022年3月连续三次凌日期间被观测到。我们对CUTE观测结果进行了分析,结果表明近紫外(2500-3300 Å)宽带传输深度(1.08−0.08+0.08%)约为视觉传输深度的两倍,表明该行星有一个扩展的、热的上层大气,温度约为15,000 K,质量损失率约为4 × 108 kg s−1。在分辨率为10 Å的透射光谱中,我们观察到Mg ii谱线(R p /R s为0.212−0.061+0.038)在罗氏波叶之外的吸收,在>4σ显著性,而在较低分辨率(100 Å)下,我们观察到一个准连续的吸收信号,与以Fe ii为主的低电离金属吸收“森林”相一致。结果表明,上层大气温度(~ 15,000 K)比目前最先进的流体动力学模型预测的要高。
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CUTE Reveals Escaping Metals in the Upper Atmosphere of the Ultrahot Jupiter WASP-189b
Ultraviolet observations of ultrahot Jupiters, exoplanets with temperatures over 2000 K, provide us with an opportunity to investigate if and how atmospheric escape shapes their upper atmosphere. Near-ultraviolet transit spectroscopy offers a unique tool to study this process owing to the presence of strong metal lines and a bright photospheric continuum as the light source against which the absorbing gas is observed. WASP-189b is one of the hottest planets discovered to date, with a dayside temperature of about 3400 K orbiting a bright A-type star. We present the first near-ultraviolet observations of WASP-189b, acquired with the Colorado Ultraviolet Transit Experiment (CUTE). CUTE is a 6U NASA-funded ultraviolet spectroscopy mission, dedicated to monitoring short-period transiting planets. WASP-189b was one of the CUTE early science targets and was observed during three consecutive transits in 2022 March. We present an analysis of the CUTE observations and results demonstrating near-ultraviolet (2500–3300 Å) broadband transit depth ( 1.08−0.08+0.08% ) of about twice the visual transit depth indicating that the planet has an extended, hot upper atmosphere with a temperature of about 15,000 K and a moderate mass-loss rate of about 4 × 108 kg s−1. We observe absorption by Mg ii lines (R p /R s of 0.212−0.061+0.038 ) beyond the Roche lobe at >4σ significance in the transmission spectrum at a resolution of 10 Å, while at lower resolution (100 Å), we observe a quasi-continuous absorption signal consistent with a “forest” of low-ionization metal absorption dominated by Fe ii. The results suggest an upper atmospheric temperature (∼15,000 K), higher than that predicted by current state-of-the-art hydrodynamic models.
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