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Measurements of the absorption and scattering coefficients of aerosol particles in suburb of Nanjing (China)

机译:南京郊区(中国)气溶胶颗粒的吸收和散射系数的测量

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The absorption and scattering coefficients of atmospheric aerosols were continuously measured with a Photoacoustic Soot Spectrometer (PASS, DMT Inc. USA) at a suburb site of Nanjing, one of the regions experiencing rapid industrialization in China. The measurements were carried out during autumn and winter 2007. A preliminary analysis of the data shows that, the scattering coefficient, B_(scat), is two to ten times larger than the absorption coefficient, B_(abs), implying that the aerosols formed/emitted in this area are more scattering than previous assumed, and can be more important in cooling the Earth-atmosphere system. The results also indicate that the absolute values of both parameters are very much dependent on the meteorological conditions, such as wind speed and direction, fog, rain, etc. as well as the time of the day. Higher values often appear at nighttimes when wind is weak, especially when a temperature inverse layer is present near the surface. Higher values of B_(scat) and B_(abs) were also observed under hazy and foggy weather conditions or when wind is blown from east, where a large industrial zone is located. Simultaneous measurements of the number concentrations, chemical compositions, and size distributions of aerosol particles are used to explain the characteristics of the changes in B_(scat) and B_(abs).
机译:在中国一个工业化迅速发展的地区之一的南京郊区,用光声煤烟光谱仪(PASS,美国DMT公司)连续测量了大气气溶胶的吸收系数和散射系数。测量是在2007年秋冬季进行的。对数据的初步分析表明,散射系数B_(scat)比吸收系数B_(abs)大2至10倍,这表明形成了气溶胶。在该区域中/散布的散射比以前的假设要多,并且在冷却地球大气系统中可能更为重要。结果还表明,这两个参数的绝对值在很大程度上取决于气象条件,例如风速和风向,雾,雨等,以及一天中的时间。较高的值通常在夜间风弱时出现,尤其是当表面附近存在逆温层时。在朦胧和多雾的天气条件下,或从大工业区所在的东部吹来风时,也观察到较高的B_(scat)和B_(abs)值。同时测量气溶胶颗粒的浓度,化学组成和尺寸分布可解释B_(scat)和B_(abs)变化的特征。

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