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首页> 外文期刊>Advances in Meteorology >Ground-Based Polarimetric Remote Sensing of Dust Aerosol Properties in Chinese Deserts near Hexi Corridor
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Ground-Based Polarimetric Remote Sensing of Dust Aerosol Properties in Chinese Deserts near Hexi Corridor

机译:河西走廊附近中国沙漠粉尘气溶胶特性的地基极化遥感。

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摘要

One-year observation of dust aerosol properties near Hexi Corridor was obtained from polarimetric measurements by ground-based sunphotometer in the county of Minqin in northwestern China from March 2012 to February 2013. We observed an annual mean AOD of0.22±0.22at 0.50 μm and Ångström exponents of 0.1–1.0 fitting a bimode normal distribution centered at 0.18 and 0.50, respectively. The effective radii of fine (0.13–0.17 μm) and coarse (2.49–3.49 μm) modes were found stable at all seasons together with the appearance of a third mode of particle radius at 0.4–1.0 μm when AOD was larger than 0.6. It is noticeable that the real (1.5–1.7) and imaginary (0.0005 to 0.09) parts of complex refractive indices were higher than other studies performed in other desert regions of China, while single scattering albedo was relatively lower (~0.84–0.89) at wavelengths of 0.44, 0.67, 0.87, and 1.02 μm. This is partially due to calcite or hematite in the soil in Minqin or the influence of anthropogenic aerosols containing carbon. Moreover, from our novel polarimetric measurement, the scattering phase function (F11) and degree of linear polarization for incident unpolarized light (-F12/F11) of dust aerosols were also obtained within this deserted area.
机译:2012年3月至2013年2月,通过对西北民勤县的地面日光光度计进行极化测量,对河西走廊附近的粉尘气溶胶特性进行了为期一年的观测。在0.50μm处,年平均AOD为0.22±0.22。和0.1–1.0的Ångström指数分别拟合以0.18和0.50为中心的双峰正态分布。精细模式(0.13–0.17μm)和粗糙模式(2.49–3.49μm)的有效半径在所有季节都稳定,并且当AOD大于0.6时,第三种模式的半径在0.4–1.0μm处出现。值得注意的是,复数折射率的实部(1.5–1.7)和虚部(0.0005至0.09)高于在中国其他沙漠地区进行的其他研究,而单散射反射率相对较低(〜0.84–0.89)。波长分别为0.44、0.67、0.87和1.02μm。这部分是由于民勤土壤中的方解石或赤铁矿或人为的含碳气溶胶的影响。此外,通过我们新颖的极化测量,在该荒漠地区还获得了粉尘气溶胶入射非偏振光的散射相位函数(F11)和线性偏振度(-F12 / F11)。

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