论文标题
移动III。同时X射线和紫外线观测揭示了热木星HD的可变环境189733b
MOVES III. Simultaneous X-ray and ultraviolet observations unveiling the variable environment of the hot Jupiter HD 189733b
论文作者
论文摘要
在第三篇动作的论文中(蒸发外部球星及其星星的多波长观察)计划,我们将哈勃太空望远镜远程望远镜观测与XMM-Newton/swift X-ray观测结合在一起,以测量各种FUV系列中HD 189733的发射。基于这些测量值,我们将星际介质朝向HD 189733并得出恒星的半合成XUV光谱,该光谱用于研究其在五个不同时期下其高能发射的演变。观察到了HD 189733的两种耀斑,但我们建议其光谱能量分布的长期变化对HD 189733B环境最重要的后果。减少的冠状和风能可以有利于在行星前的弓震中形成密集的Si $^{2+} $原子,负责在前两个时期测量的前和透射吸收。在第二,第三和第五个时期的Lyman-$α$线中检测到传播吸收特征,这可能是由扩展的行星热圈和恒星风质质子的尾巴与行星外层中的电荷交换中和恒星风质子的尾部产生的。我们建议,地球的X射线照射增加,并减少其EUV辐照,从而导致中性氢的光电离率较低,从而通过维持较大的H $^{0} $原子在上层大气中的较大密度来检测这些特征,并在上层大气层中与Stellar the Stellar风中的增强式电荷。在上一个时期,更深宽,更广泛的吸收特征表明,行星进入了不同的蒸发方案,为恒星活动与行星环境结构之间的联系提供了线索。
In this third paper of the MOVES (Multiwavelength Observations of an eVaporating Exoplanet and its Star) programme, we combine Hubble Space Telescope far-ultraviolet observations with XMM-Newton/Swift X-ray observations to measure the emission of HD 189733 in various FUV lines, and its soft X-ray spectrum. Based on these measurements we characterise the interstellar medium toward HD 189733 and derive semi-synthetic XUV spectra of the star, which are used to study the evolution of its high-energy emission at five different epochs. Two flares from HD 189733 are observed, but we propose that the long-term variations in its spectral energy distribution have the most important consequences for the environment of HD 189733b. Reduced coronal and wind activity could favour the formation of a dense population of Si$^{2+}$ atoms in a bow-shock ahead of the planet, responsible for pre- and in-transit absorption measured in the first two epochs. In-transit absorption signatures are detected in the Lyman-$α$ line in the second, third and fifth epochs, which could arise from the extended planetary thermosphere and a tail of stellar wind protons neutralised via charge-exchange with the planetary exosphere. We propose that increases in the X-ray irradiation of the planet, and decreases in its EUV irradiation causing lower photoionisation rates of neutral hydrogen, favour the detection of these signatures by sustaining larger densities of H$^{0}$ atoms in the upper atmosphere and boosting charge-exchanges with the stellar wind. Deeper and broader absorption signatures in the last epoch suggest that the planet entered a different evaporation regime, providing clues as to the link between stellar activity and the structure of the planetary environment.