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实验室水云的液滴尺寸光谱和水汽浓度:傅里叶变换红外(500 - 5000厘米⁻¹)光学深度测量的反演

Droplet size spectra and water-vapor concentration of laboratory water clouds: inversion of Fourier transform infrared (500-5000 cm(-1)) optical-depth measurement.

作者信息

Arnott W P, Schmitt C, Liu Y, Hallett J

出版信息

Appl Opt. 1997 Jul 20;36(21):5205-16. doi: 10.1364/ao.36.005205.

Abstract

Infrared extinction optical depth (500-5000 cm(-1)) has been measured with a Fourier transform infrared spectrometer for clouds produced with an ultrasonic nebulizer. Direct measurement of the cloud droplet size spectra agree with size spectra retrieved from inversion of the extinction measurements. Both indicate that the range of droplet sizes is 1-14 mum. The retrieval was accomplished with an iterative algorithm that simultaneously obtains water-vapor concentration. The basis set of droplet extinction functions are computed once by using numerical integration of the Lorenz-Mie theory over narrow size bins, and a measured water-vapor extinction curve was used. Extinction and size spectra are measured and computed for both steady-state and dissipating clouds. It is demonstrated that anomalous diffraction theory produces relatively poor droplet size and synthetic extinction spectra and that extinction measurements are helpful in assessing the validity of various theories. Calculations of cloud liquid-water content from retrieved size distributions agree with a parameterization based on optical-depth measurements at a wave number of 906 cm(-1) for clouds that satisfy the size spectral range assumptions of the parameterization. Significance of droplet and vapor contribution to the total optical depth is used to evaluate the reliability of spectral inversions.

摘要

利用傅里叶变换红外光谱仪测量了超声雾化器产生的云的红外消光光学深度(500 - 5000 cm⁻¹)。对云滴尺寸谱的直接测量结果与通过消光测量反演得到的尺寸谱一致。两者均表明液滴尺寸范围为1 - 14μm。反演是通过一种同时获取水汽浓度的迭代算法完成的。液滴消光函数的基集通过在窄尺寸区间上对洛伦兹 - 米理论进行数值积分计算一次得到,并使用了实测的水汽消光曲线。对稳态云和消散云都进行了消光和尺寸谱的测量与计算。结果表明,反常衍射理论给出的液滴尺寸和合成消光谱相对较差,消光测量有助于评估各种理论的有效性。从反演得到的尺寸分布计算出的云液水含量,与基于906 cm⁻¹波数处光学深度测量的参数化结果一致,该参数化适用于满足其尺寸谱范围假设的云。利用液滴和水汽对总光学深度的贡献的重要性来评估光谱反演的可靠性。

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