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Ground-based optical transmission spectrum of the hot Jupiter HAT-P-1b

机译:热木星HAT-P-1b的地面光传输光谱 <相关对象object-type =“ tableCDS” source-id = “ http://cdsarc.u-strasbg.fr/viz-bin/cat/J/A+A/631/A169” source-id-type =“ url” />

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Context. Time-series spectrophotometric studies of exoplanets during transit using ground-based facilities are a promising approach to characterize their atmospheric compositions. Aims. We aim to investigate the transit spectrum of the hot Jupiter HAT-P-1b. We compare our results to those obtained at similar wavelengths by previous space-based observations. Methods. We observed two transits of HAT-P-1b with the Gemini Multi-Object Spectrograph (GMOS) instrument on the Gemini North telescope using two instrument modes covering the 320–800 and 520–950 nm wavelength ranges. We used time-series spectrophotometry to construct transit light curves in individual wavelength bins and measure the transit depths in each bin. We accounted for systematic effects. We addressed potential photometric variability due to magnetic spots in the planet’s host star with long-term photometric monitoring. Results. We find that the resulting transit spectrum is consistent with previous Hubble Space Telescope (HST) observations. We compare our observations to transit spectroscopy models that marginally favor a clear atmosphere. However, the observations are also consistent with a flat spectrum, indicating high-altitude clouds. We do not detect the Na resonance absorption line (589 nm), and our observations do not have sufficient precision to study the resonance line of K at 770 nm. Conclusions. We show that even a single Gemini/GMOS transit can provide constraining power on the properties of the atmosphere of HAT-P-1b to a level comparable to that of HST transit studies in the optical when the observing conditions and target and reference star combination are suitable. Our 520–950 nm observations reach a precision comparable to that of HST transit spectra in a similar wavelength range of the same hot Jupiter, HAT-P-1b. However, our GMOS transit between 320–800 nm suffers from strong systematic effects and yields larger uncertainties.
机译:上下文。使用地面设施对系外行星进行转运的时间序列分光光度法研究是表征其大气成分的有前途的方法。目的我们旨在研究热木星HAT-P-1b的传输光谱。我们将我们的结果与以前的空基观测在相似波长下获得的结果进行比较。方法。我们使用Gemini North望远镜上的Gemini多目标光谱仪(GMOS)仪器观察了HAT-P-1b的两次跃迁,该仪器使用了涵盖320–800和520–950 nm波长范围的两种仪器模式。我们使用时间分光光度法在各个波长仓中构建了过渡光曲线,并测量了每个仓中的过渡深度。我们考虑了系统的影响。我们通过长期的光度监测解决了由于行星宿主恒星中的磁点引起的潜在光度变异性。结果。我们发现产生的传输光谱与先前的哈勃太空望远镜(HST)观测结果一致。我们将我们的观察结果与过境光谱模型进行了比较,后者只是偏向于一个晴朗的大气层。但是,这些观测结果也与平坦的频谱一致,表明出现了高空云。我们没有检测到Na共振吸收线(589 nm),并且我们的观察结果还不足以研究770 nm K的共振线。结论。我们显示,当观测条件以及目标星和参考星的组合为时,即使在一次单子双星/ GMOS传播过程中,对HAT-P-1b大气性质的抑制能力也可以与在光学中的HST跃迁研究相当。适当。在相同的热木星HAT-P-1b的相似波长范围内,我们的520-950 nm观测值达到了与HST传输光谱相当的精度。但是,我们在320-800 nm之间的GMOS传输受到强大的系统影响,并产生更大的不确定性。

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