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Impact of atmospheric circulations on aerosol distributions in autumn over eastern China: observational evidence

机译:大气环流对中国东部秋季秋季气溶胶分布的影响:观测证据

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Regional heavy pollution events in eastern China (110-122 degrees E, 28-40 degrees N) are causing serious environmental problems. In this study, the relationship between the degree of regional pollution and the patterns of large-scale atmospheric circulation over eastern China in October is investigated using 10-year (2001-2010) Terra/MODIS aerosol optical depth and NCEP reanalysis data by both case study and composite analysis. Eighteen polluted and 10 clean episodes are selected and categorised into six polluted types and three clean types respectively. Generally speaking, weather patterns such as a uniform surface pressure field in eastern China or a steady straight westerly in the middle troposphere, particularly when being at the rear of the anticyclone at 850 hPa, are typically responsible for heavy pollution events. Meanwhile, clean episodes occur when strong southeastward cold air advection prevails below the middle troposphere or air masses are transported from sea to land. Uniform descending motion prevails over the study region, trapping pollutants in the lower atmosphere. Therefore, the value of vertical velocity averaged from 1000 to 100 hPa and divergence of wind field in the lower troposphere are used in this study to quantify the diffusion conditions in each circulation type. The results reveal that it is often a clean episode when both the mean downward motion (larger than 2.56 x 10(-2) Pa s(-1)) and the divergence of low-level winds (larger than 1.79 x 10(-2) s(-1)) are strong. Otherwise, it is more likely to be a polluted episode.
机译:中国东部地区(东经110-122度,北纬28-40度)的重度污染事件正在引起严重的环境问题。在这项研究中,使用10年(2001-2010年)Terra / MODIS气溶胶光学深度和NCEP再分析数据,研究了10月份中国东部区域污染程度与大规模大气环流模式之间的关系。研究和综合分析。选择18个污染事件和10个清洁事件,分别分为6种污染类型和3种清洁类型。一般而言,天气模式,例如中国东部的均匀表面压力场​​或对流层中部的平直西风,特别是在850 hPa位于反气旋后部时,通常是造成严重污染事件的原因。同时,当对流层中层以下向东南方向强烈向南平流盛行或空气团从海向陆输送时,就会发生干净的事件。均匀的下降运动在研究区域内普遍存在,将污染物捕获在较低的大气层中。因此,本研究使用平均速度为1000至100 hPa的值和对流层下部的风场发散来量化每种循环类型中的扩散条件。结果表明,当平均向下运动(大于2.56 x 10(-2)Pa s(-1))和低水平风的发散(大于1.79 x 10(-2)时,这通常是干净的情节。 )s(-1))很强。否则,很可能是污染事件。

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