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arXiv 1904.09986astro-ph.EPastro-ph.SR
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含碳氢化合物雾的系外行星大气的理论透射谱。II。UV辐照强度、金属性、C/O比、涡流扩散系数和温度的依赖性

Theoretical Transmission Spectra of Exoplanet Atmospheres with Hydrocarbon Haze. II. Dependence on UV Irradiation Intensity, Metallicity, C/O Ratio, Eddy Diffusion Coefficient, and Temperature

Yui Kawashima, Masahiro Ikoma

摘要:

最近的透射光谱显示,云和薄雾在近距离系外行星的大气中很常见。在这项研究中,使用光化学,微物理和透射光谱模式的近距离温暖,($\lesssim$ 1000 K)系外行星大气,我们在我们的前一篇论文中新开发的(Kawashima & Ikoma 2018),我们研究了雾霾颗粒和气态物质的垂直分布,以及在宽范围的模型参数(包括紫外辐射强度,金属含量,碳氧比(C/O)、涡流扩散系数和温度。对金属丰度的敏感性特别令人感兴趣。我们发现,金属丰度的上升基本上导致烃的光解离速率降低,因此降低了混浊单体的产生速率。这是由于存在于比碳氢化合物更高的海拔处的主要光子吸收剂(例如$\mathrm{H_2O}$、$\mathrm{CO}$、$\mathrm{CO_2}$和$\mathrm{O_2}$)的增强的光子屏蔽效应。我们还发现,在相对较短的波长($\lesssim$ 2-3 $μ$ m),在透射光谱中的吸收功能是最明显的中等金属丰度,如100倍的太阳金属丰度,而较低的金属丰度较强的吸收功能在相对较长的波长($\gtrsim$ 2-3 $μ$ m),其中霾的贡献很小。这是因为两个竞争性的影响,降低烟雾的生产率和大气尺度的高度较高的金属。对于其他模型参数,我们发现,较强的吸收功能出现在较低的紫外线照射,较低的C/O比,较高的涡流扩散系数,和较高的温度的大气的透射光谱。

英文摘要:

Recent transmission spectroscopy has revealed that clouds and hazes are common in the atmospheres of close-in exoplanets. In this study, using the photochemical, microphysical, and transmission spectrum models for close-in warm ($\lesssim$ 1000 K) exoplanet atmospheres that we newly developed in our preceding paper (Kawashima & Ikoma 2018), we investigate the vertical distributions of haze particles and gaseous species and the resultant transmission spectra over wide ranges of the model parameters including UV irradiation intensity, metallicity, carbon-to-oxygen ratio (C/O), eddy diffusion coefficient, and temperature. The sensitivity to metallicity is of particular interest. We find that a rise in metallicity leads basically to reducing the photodissociation rates of the hydrocarbons and therefore the haze monomer production rates. This is due to an enhanced photon-shielding effect by the major photon absorbers such as $\mathrm{H_2O}$, $\mathrm{CO}$, $\mathrm{CO_2}$, and $\mathrm{O_2}$, existing at higher altitudes than the hydrocarbons. We also find that at relatively short wavelengths ($\lesssim$ 2-3 $μ$m), the absorption features in transmission spectra are most pronounced for moderate metallicities such as 100 times the solar metallicity, whereas the lower the metallicity the stronger the absorption features at relatively long wavelengths ($\gtrsim$ 2-3 $μ$m), where the contribution of haze is small. These are because of the two competing effects of reduced haze production rate and atmospheric scale height for higher metallicities. For the other model parameters, we show that stronger absorption features appear in transmission spectra of the atmospheres with lower UV irradiation, lower C/O ratio, higher eddy diffusion coefficient, and higher temperature.

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