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[论文解读] The GROUSE project II: Detection of the Ks-band secondary eclipse of exoplanet HAT-P-1b

Ernst de Mooij, Remco de Kok|arXiv (Cornell University)|Feb 28, 2011
Stellar, planetary, and galactic studies参考文献 30被引用 45
一句话总结

本研究利用威廉·赫歇尔望远镜上的LIRIS仪器,首次在地基观测中检测到系外行星HAT-P-1b在Ks波段的二次凌日,测得2.2 μm处的凌日深度为0.109 ± 0.025%,对应亮度温度为2136+150−170 K。结果表明其温度显著高于标准大气模型的预测值,挑战了当前对热木星能量收支的理解,提示可能存在系统误差或未被考虑的大气过程。

ABSTRACT

Context: Only recently it has become possible to measure the thermal emission from hot-Jupiters at near-Infrared wavelengths using ground-based telescopes, by secondary eclipse observations. This allows the planet flux to be probed around the peak of its spectral energy distribution, which is vital for the understanding of its energy budget. Aims: The aim of the reported work is to measure the eclipse depth of the planet HAT-P-1b at 2.2micron. This planet is an interesting case, since the amount of stellar irradiation it receives falls in between that of the two best studied systems (HD209458 and HD189733), and it has been suggested to have a weak thermal inversion layer. Methods: We have used the LIRIS instrument on the William Herschel Telescope (WHT) to observe the secondary eclipse of HATP-1b in the Ks-band, as part of our Ground-based secondary eclipse (GROUSE) project. The observations were done in staring mode, while significantly defocusing the telescope to avoid saturation on the K=8.4 star. With an average cadence of 2.5 seconds, we collected 6520 frames during one night. Results: The eclipse is detected at the 4sigma level, the measured depth being 0.109+/-0.025%. The uncertainties are dominated by residual systematic effects, as estimated from different reduction/analysis procedures. The measured depth corresponds to a brightness temperature of 2136+150-170K. This brightness temperature is significantly higher than those derived from longer wavelengths, making it difficult to fit all available data points with a plausible atmospheric model. However, it may be that we underestimate the true uncertainties of our measurements, since it is notoriously difficult to assign precise statistical significance to a result when systematic effects are important.

研究动机与目标

  • 利用地基红外测光技术,在2.2 μm波段测量HAT-P-1b的热辐射,探测其昼面能量收支,接近其光谱能量分布的峰值波长。
  • 检验观测到的凌日深度是否能通过包含或不包含温度反转的典型大气模型加以解释。
  • 探究云层或其他大气组分在解释观测与模型之间Ks波段通量差异中的作用。
  • 评估系统误差对地基系外行星二次凌日观测中测光精度的影响。

提出的方法

  • 观测采用威廉·赫歇尔望远镜上的LIRIS红外相机,以凝视模式进行,通过显著离焦避免K=8.4等的恒星饱和。
  • 单夜观测共获取6,520帧,平均时间采样间隔为2.5秒。
  • 使用多个数据处理与分析流程对测光时间序列进行处理,以估计主要由残余系统效应主导的不确定性。
  • 利用相关k方法计算大气模型,采用不同的温度-压力分布、成分(包括H2O、CO、CO2、CH4)以及具有金星特性(光学厚度1.5,1-μm粒子)的云层。
  • 将模型预测结果以0.1 μm分辨率进行重采样,并与Ks、L波段及斯皮兹曼望远镜波段的观测凌日深度进行对比,以评估拟合优度。
  • 根据测得的凌日深度推导亮度温度,并在系统误差占主导地位的情况下评估结果的统计显著性。

实验结果

研究问题

  • RQ1地基望远镜能否以足够精度检测HAT-P-1b在Ks波段的二次凌日,从而约束其热辐射?
  • RQ2为何测得的Ks波段亮度温度显著高于长波段斯皮兹曼观测所推导的值?
  • RQ3包含或不包含温度反转的典型无云大气模型能否重现观测到的Ks波段凌日深度?
  • RQ4具有金星特性(光学厚度1.5)的云层是否能改善模型在多波段观测数据上的拟合效果?
  • RQ5测光数据处理中的系统效应在多大程度上导致了凌日深度的观测偏差?

主要发现

  • 在Ks波段以4-σ显著性水平检测到HAT-P-1b的二次凌日,测得凌日深度为0.109 ± 0.025%。
  • 推导出的亮度温度为2136+150−170 K,显著高于由长波段斯皮兹曼观测推导出的值。
  • 在标准气体丰度(H2O、CO、CO2、CH4)下,任何合理的无云大气模型均无法同时拟合Ks波段与斯皮兹曼数据,尤其考虑到Ks波段吸收较弱。
  • 在对流层顶处具有光学厚度1.5的金星型云层可改善对Ks波段深度的拟合,但其成分在热木星大气中缺乏物理解释。
  • 偏差可能源于测光数据处理中持续存在的系统效应导致的不确定性被低估,从而对结果的统计显著性构成挑战。
  • 结果表明,当前大气模型尚无法解释HAT-P-1b完整的光谱能量分布,提示在能量再分配或云物理机制方面可能存在理解上的空白。

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