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首页> 外文期刊>The Astrophysical journal >A New Search for Carbon Monoxide Absorption in the Transmission Spectrum of the Extrasolar Planet HD 209458b*
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A New Search for Carbon Monoxide Absorption in the Transmission Spectrum of the Extrasolar Planet HD 209458b*

机译:在太阳系外行星HD 209458b的透射光谱中寻找一氧化碳吸收的新方法*

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We have revisited the search for carbon monoxide absorption features in transmission during the transit of the extrasolar planet HD 209458b. In 2002 August-September we acquired a total of 1077 high-resolution spectra (λ/δλ ~ 25,000) in the K-band (2 μm) wavelength region using NIRSPEC on the Keck II telescope during three transits. These data are more numerous and of better quality than the data analyzed in an initial search by Brown et al. Our analysis achieves a sensitivity sufficient to test the degree of CO absorption in the first-overtone bands during transit on the basis of plausible models of the planetary atmosphere. We analyze our observations by comparison with theoretical tangent geometry absorption spectra, computed by adding height-invariant ad hoc temperature perturbations to the model atmosphere of Sudarsky et al. and by treating cloud height as an adjustable parameter. We do not detect CO absorption. The strong 2-0 R-branch lines between 4320 and 4330 cm-1 have depths during transit less than 1.6 parts in 104 in units of the stellar continuum (3 σ limit) at a spectral resolving power of 25,000. Our analysis indicates a weakening similar to that found in the case of sodium, suggesting that a general masking mechanism is at work in the planetary atmosphere. Under the interpretation that this masking is provided by high clouds, our analysis defines the maximum cloud-top pressure (i.e., minimum height) as a function of the model atmospheric temperature. For the relatively hot model used by Charbonneau et al. to interpret their sodium detection, our CO limit requires cloud tops at or above 3.3 mbar, and these clouds must be opaque at a wavelength of 2 μm. High clouds comprised of submicron-sized particles are already present in some models but may not provide sufficient opacity to account for our CO result. Cooler model atmospheres, having smaller atmospheric scale heights and lower CO mixing ratios, may alleviate this problem to some extent. However, even models 500 K cooler than the Sudarsky et al. model require clouds above the 100 mbar level to be consistent with our observations. Our null result therefore requires clouds to exist at an observable level in the atmosphere of HD 209458b, unless this planet is dramatically colder than current belief.
机译:我们已经重新研究了太阳系外行星HD 209458b的传输过程中对一氧化碳吸收特性的搜索。在2002年8月至9月,我们使用了Keck II望远镜上的NIRSPEC在3个传输过程中在K波段(2μm)波长范围内获得了总计1077个高分辨率光谱(λ/δλ〜25,000)。这些数据比Brown等人在最初的搜索中分析的数据更多,质量更高。我们的分析获得了足够的灵敏度,可以根据合理的行星大气模型测试运输过程中第一泛音带中的CO吸收程度。我们通过与理论切线几何吸收光谱进行比较来分析我们的观测结果,该理论是通过将高度不变的临时温度扰动添加到Sudarsky等人的模型大气中来计算的。并将云的高度视为可调参数。我们没有检测到CO吸收。在4320和4330 cm-1之间的强2-0 R分支线在传输过程中的深度小于2分之恒星连续体(3σ极限)中104的1.6份,光谱分辨力为25,000。我们的分析表明,这种减弱与钠的情况相似,这表明行星大气中存在一种通用的掩盖机制。根据这种掩盖是由高云提供的解释,我们的分析将最大云顶压力(即最小高度)定义为模型大气温度的函数。对于Charbonneau等人使用的相对较热的模型。为了解释其钠含量检测,我们的CO限值要求云顶在3.3 mbar或更高,并且这些云在2μm的波长下必须是不透明的。在某些模型中已经存在由亚微米级颗粒组成的高云,但是可能无法提供足够的不透明度来说明我们的CO结果。具有较小大气尺度高度和较低CO混合比的凉爽模型大气可以在某种程度上缓解此问题。但是,即使模型比Sudarsky等人的模型低500K。该模型要求100 mbar以上的云层与我们的观察一致。因此,我们的无效结果要求在HD 209458b的大气层中以可观察的水平存在云,除非该行星比当前的信念明显更冷。

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