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arXiv 2007.00109astro-ph.EP
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JWST光谱II:云雾状系外行星的限制气溶胶种类、粒度分布、温度和金属丰度

JWST Transit Spectra II: Constraining Aerosol Species, Particle-size Distributions, Temperature, and Metallicity for Cloudy Exoplanets

Brianna Lacy, Adam Burrows

摘要:

JWST将首次提供从光学到中红外的连续波长覆盖的中等分辨率过境光谱。在本文中,我们说明了不同的气溶胶种类,尺寸分布和空间分布编码信息JWST过境光谱。我们使用过境光谱建模代码METIS,随着米氏理论和几个灵活的处理气溶胶的大小和空间分布进行参数敏感性研究,计算过境贡献函数,计算雅可比矩阵,并检索参数与马尔可夫链蒙特卡罗。更广泛的波长覆盖范围的JWST将可能包括足够的非灰色气溶胶的行为,以恢复有关粒子的种类和尺寸分布的信息,特别是如果从气溶胶产生的独特的共振功能存在。在JWST波长范围内,光学和中红外通常提供关于0.1-1 $μ$ m大小的气溶胶的信息,而近红外到中红外波长通常提供关于气体吸收的信息,即使存在气溶胶。红外线中强烈的气体吸收特征通常仍然可见,即使当云和薄雾使目前可观察到的光谱的光学和近红外部分变平时。对于气溶胶性质、温度和表面重力的某些组合,尽管存在气溶胶,人们仍然可以精确测量金属丰度,但更常见的是,多云或朦胧大气的检索金属丰度的精确度显着低于具有类似性质的晴朗大气。未来的努力,以安全地链接气溶胶性质的大气金属丰度和温度在物理动机的方式将最终使一个强大的物理理解的过程中发挥作用,在多云,朦胧的系外行星大气。

英文摘要:

JWST will provide moderate resolution transit spectra with continuous wavelength coverage from the optical to the mid-infrared for the first time. In this paper, we illustrate how different aerosol species, size-distributions, and spatial distributions encode information in JWST transit spectra. We use the transit spectral modeling code METIS, along with Mie theory and several flexible treatments of aerosol size and spatial distributions to perform parameter sensitivity studies, calculate transit contribution functions, compute Jacobians, and retrieve parameters with Markov Chain Monte Carlo. The broader wavelength coverage of JWST will likely encompass enough non-gray aerosol behavior to recover information about the species and size-distribution of particles, especially if distinct resonance features arising from the aerosols are present. Within the JWST wavelength range, the optical and mid-infrared typically provide information about 0.1-1 $μ$m sized aerosols, while the near-infrared to mid-infrared wavelengths usually provide information about gaseous absorption, even if aerosols are present. Strong gaseous absorption features in the infrared often remain visible, even when clouds and hazes are flattening the optical and NIR portion of the spectrum that is currently observable. For some combinations of aerosol properties, temperature, and surface gravity, one can make a precise measure of metallicity despite the presence of aerosols, but more often the retrieved metallicity of a cloudy or hazy atmosphere has significantly lower precision than for a clear atmosphere with otherwise similar properties. Future efforts to securely link aerosol properties to atmospheric metallicity and temperature in a physically motivated manner will ultimately enable a robust physical understanding of the processes at play in cloudy, hazy exoplanet atmospheres.

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