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Light absorption from particulate impurities in snow and ice determined by spectrophotometric analysis of filters

机译:通过滤光片的分光光度法测定雪和冰中颗粒杂质的吸光度

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Light absorption by particulate impurities in snow and ice can affect the surface albedo and is important for the climate. The absorption properties of these particles can be determined by collecting and melting snow samples and extracting the particulate material by filtration of the meltwater. This paper describes the optical design and testing of a new instrument to measure the absorption spectrum from 400 to 750 nm wavelength of the particles collected on filters using an "integrating-sandwich" configuration. The measured absorption is shown to be unaffected by scattering of light from the deposited particulates. A set of calibration standards is used to derive an upper limit for the concentration of black carbon (BC) in the snow. The wavelength dependence of the absorption spectra from 450 to 600 nm is used to calculate an absorption Angstrom exponent for the aerosol. This exponent is used to estimate the actual BC concentration in the snow samples as well as the relative contributions of BC and non-BC constituents to the absorption of solar radiation integrated over the wavelength band 300 to 750 nm.
机译:雪和冰中的颗粒杂质吸收的光会影响地表反照率,对气候非常重要。这些颗粒的吸收特性可以通过收集和融化雪样并通过过滤融水来提取颗粒材料来确定。本文介绍了一种新仪器的光学设计和测试,该仪器使用“积分夹心”配置来测量从滤光片收集的颗粒的400至750 nm波长的吸收光谱。显示出所测量的吸收不受沉积颗粒的光散射的影响。一组校准标准用于得出雪中黑碳(BC)浓度的上限。从450到600 nm的吸收光谱的波长依赖性用于计算气雾剂的吸收埃指数。该指数用于估计积雪样本中的实际BC浓度以及BC和非BC成分对在300至750 nm波长范围内积分的太阳辐射吸收的相对贡献。

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