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ISSN 1006-9895

CN 11-1768/O4

人为大气污染物对一次冬季浓雾形成发展的影响研究
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公益性行业 (气象) 科研专项GYHY200806001,国家科技支撑计划2006BAC12B03


Impacts of Anthropogenic Atmospheric Pollutant on Formation and Development of a Winter Heavy Fog Event
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    摘要:

    基于WRF/Chem模式和雾的观测资料,开展了包含和不包含人为污染排放源两种大气背景条件下的数值模拟对比试验,在此基础上探讨了人为污染物对2009年12月1日发生在我国华北和华东地区的一次浓雾天气过程的影响机理.结果表明,在考虑污染排放源时,模式模拟的雾的空间分布和强度变化与卫星、能见度仪和微波辐射计的观测更为接近.污染条件下的边界层结构更有利于雾的形成,人为大气污染物使雾的范围最大增加50%,雾的强度最大增加5倍,平均延长雾持续时间1.5小时.由于人为污染物增加了雾凝结核 (FCN) 数浓度,进而使雾滴数浓度显著增大,有利于雾的增强.同时,污染物通过影响雾滴的凝结过程和潜热释放过程,对长波辐射降温和湍流过程有重要影响,使边界层的热力和动力结构更有利于雾的增强和发展.污染气体SO2、NOx和NH3的排放产生的二次气溶胶对雾的形成和发展具有重要影响.不考虑这些污染气体排放时,平均雾水含量可降低32%.

    Abstract:

    The WRF/Chem model coupled with local anthropogenic atmospheric pollution emissions and fog observational data were used to assess the effects of human-induced pollutants on a heavy fog event on 1 Dec 2009 in North China and East China. The experiments with and without anthropogenic emissions were designed and conducted. The results suggest that the simulated fog distribution and intensity with anthropogenic emission are closer to observed ones. The polluted atmospheric boundary condition is found to create a favorable condition for fog formation, increasing the fog area up to 50%, the intensity of 5 times in maximum, and the duration of 1.5 h on average. Compared with that under clean air condition, the number concentration of fog condensation nuclei (FCN) is much higher in polluted air, which causes a higher fog droplet number concentration, and influences the processes of droplet condensation, long wave radiation, turbulent motion, and provides the favorable dynamic and thermal boundary conditions for fog development. The secondary aerosols produced by trace gases SO2, NOx, and NH3 make great influence on the formation and development of fog, and the averaged liquid water content has a decrease of 32%, without these trace gas emission.

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贾星灿,郭学良.人为大气污染物对一次冬季浓雾形成发展的影响研究.大气科学,2012,36(5):995~1008 JIA Xingcan, GUO Xueliang. Impacts of Anthropogenic Atmospheric Pollutant on Formation and Development of a Winter Heavy Fog Event. Chinese Journal of Atmospheric Sciences (in Chinese),2012,36(5):995~1008

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  • 收稿日期:2011-10-26
  • 最后修改日期:2012-03-08
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  • 在线发布日期: 2012-09-19
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