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Infrared complex refractive indices of supercooled liquid HNO_3/H_2O aerosols

机译:过冷液态HNO_3 / H_2O气溶胶的红外复折射率

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Complex refractive indices have been retrieved for the first time directly from the Fourier transform infrared extinction spectra of supercooled liquid HNO_3/H_2O aerosols at 220 K. Aerosol compositions were determined by simultaneously monitoring equilibrium HNO_3 and H_2O vapor pressures with a tunable diode laser. The new optical constants are compared with previous results from room temperature bulk solutions and < 160 K amorphous solid thin films, and the differences are explained primarily in terms of the temperature-dependent dissociation of molecular HNO_3 into its constituent ions. Mie scattering analysis of aerosol extinction spectra suggests that using either the room temperature liquid or the amorphous solid refractive indices may result in inaccurate particle size determination. These new data sets are directly applicable to the characterization of polar stratospheric clouds though spectroscopic remote sensing.
机译:首次直接从220 K过冷液态HNO_3 / H_2O气溶胶的傅立叶变换红外消光光谱中首次获得了复折射率。通过使用可调二极管激光器同时监测平衡HNO_3和H_2O蒸气压来确定气溶胶成分。将新的光学常数与室温本体溶液和<160 K无定形固体薄膜的先前结果进行了比较,并主要根据温度依赖性分子HNO_3分解为其组成离子的方式来解释差异。气溶胶消光光谱的米氏散射分析表明,使用室温液体或无定形固体折射率可能导致粒度测定不准确。这些新的数据集可通过光谱遥感直接用于表征平流层极地云。

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