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首页> 外文期刊>Atmospheric chemistry and physics >Dust events in Beijing, China (2004-2006): Comparison of ground-based measurements with columnar integrated observations
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Dust events in Beijing, China (2004-2006): Comparison of ground-based measurements with columnar integrated observations

机译:中国北京的沙尘事件(2004年至2006年):地面观测与柱状综合观测的比较

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摘要

Ambient particle number size distributions spanning three years were used to characterize the frequency and intensity of atmospheric dust events in the urban areas of Beijing, China in combination with AERONET sun/sky radiometer data. Dust events were classified into two types based on the differences in particle number and volume size distributions and local weather conditions. This categorization was confirmed by aerosol index images, columnar aerosol optical properties, and vertical potential temperature profiles. During the type-1 events, dust particles dominated the total particle volume concentration (< 10 μm), with a relative share over 70%. Anthropogenic particles in the Aitken and accumulation mode played a subordinate role here because of high wind speeds (>4ms~(-1)). The type-2 events occurred in rather stagnant air masses and were characterized by a lower volume fraction of coarse mode particles (on average, 55%). Columnar optical properties showed that the superposition of dust and anthropogenic aerosols in type-2 events resulted in a much higher AOD (average: 1.51) than for the rather pure dust aerosols in type-1 events (average AOD: 0.36). A discrepancy was found between the groundbased and column integrated particle volume size distributions, especially for the coarse mode particles. This discrepancy likely originates from both the limited comparability of particle volume size distributions derived from Sun photometer and in situ number size distributions, and the inhomogeneous vertical distribution of particles during dust events.
机译:结合AERONET的太阳/天空辐射计数据,使用三年来的环境粒子数大小分布来表征中国北京市区大气尘埃事件的频率和强度。根据颗粒数量和体积大小分布以及当地天气条件的差异,将沙尘事件分为两种类型。通过气雾指数图像,柱状气溶胶光学特性和垂直电势温度曲线证实了这一分类。在类型1事件中,粉尘颗粒占总颗粒体积浓度(<10μm)占主导,相对份额超过70%。由于高风速(> 4ms〜(-1)),在Aitken和累积模式下的人为颗粒在这里起次要作用。 2型事件发生在停滞不前的空气质量中,其特征是较低的粗模式颗粒体积分数(平均为55%)。柱状光学特性表明,与2型事件中相当纯的粉尘气溶胶(平均AOD:0.36)相比,2型事件中的尘埃和人为气溶胶的叠加产生了更高的AOD(平均值:1.51)。发现地面和色谱柱的整体颗粒体积尺寸分布之间存在差异,尤其是对于粗模式颗粒而言。这种差异可能源于从太阳光度计得出的粒径分布和原位数粒径分布的可比性有限,以及尘埃事件期间颗粒的垂直分布不均匀。

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