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Characteristics of urban boundary layer in heavy haze process based on Beijing 325m tower data
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  • 英文篇名:Characteristics of urban boundary layer in heavy haze process based on Beijing 325m tower data
  • 作者:SHI ; Yu ; HU ; Fei ; ; Rui ; HE ; Yuanyuan
  • 英文作者:SHI Yu;HU Fei;Lü Rui;HE Yuanyuan;State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences;College of Earth and Planetary Sciences, University of Chinese Academy of Sciences;
  • 关键词:大气边界层 ; 雾霾 ; 空气污染 ; 湍流
  • 英文关键词:Atmospheric boundary layer;;haze;;air pollution;;turbulence
  • 中文刊名:AOSL
  • 英文刊名:大气和海洋科学快报(英文版)
  • 机构:State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences;College of Earth and Planetary Sciences, University of Chinese Academy of Sciences;
  • 出版日期:2019-01-16
  • 出版单位:Atmospheric and Oceanic Science Letters
  • 年:2019
  • 期:v.12
  • 基金:Supported by the National Key Research and Development Program of China [grant numbers 2017YFC0209600 and 2016YFC0208802]
  • 语种:英文;
  • 页:AOSL201901006
  • 页数:9
  • CN:01
  • ISSN:11-5693/P
  • 分类号:43-51
摘要
2015年11月24日至2015年12月2日北京市经历了一次严重的雾霾污染过程。本文利用这次过程期间北京325米气象塔的观测资料,对重污染天气条件下的边界层风场、温度场、湿度场和湍流特征进行了分析研究。本次污染过程并未发布红色预警,但是实际的污染形势被低估了,本文也对低估原因进行了分析。结果表明:北京地区这次污染过程主要是由偏东风和偏南风引起的,11月29日高层(280米)风速增加而低层(15m)风速并未增加,且次日高层风速大幅减小,导致了对于这次污染形势的低估。风速、湍动动能和摩擦速度与PM2.5浓度呈反相关关系。在晴天,风速随高度的增加而显著增加,但在污染严重的时期,风速从近地层到塔顶的变化不是很大。湍流动能从近地层到铁塔高层的变化并不是很明显。雾霾过程通常伴随有逆温层的出现,边界层内温度的日变化很小。在严重污染时,相对湿度接近100%,此时感热通量和水汽通量也都减小,湍流活动受到抑制,湍流活动强度的减弱又会进一步加重污染形势。
        Beijing experienced serious haze pollution from 24 November 2015 to 2 December 2015. To investigate the planetary boundary layer characteristics, especially turbulence characteristics, the authors analyzed the wind, temperature, humidity, and turbulence characteristics during heavily polluted weather by using the observational data of the 325-m meteorological tower in Beijing.The results indicate that the pollution was mainly caused by the easterly and southerly winds.There were negative correlations between wind speed, turbulent kinetic energy, friction velocity,and the PM2.5 concentration. During clean days, the wind speed greatly enhanced with height;however, during the period of heavy pollution, the wind speed changed a little from the nearsurface layer to the top of the tower. In contrast, the spatial variability of TKE from the nearsurface layer to the upper layer was not so obvious. The heavy haze pollution in this study was often characterized by the emergence of an inversion layer; therefore, the diurnal variation of the boundary layer temperature was very small. At the time of serious pollution, the relative humidity was near 100%. The diurnal variations of sensible heat ?ux and water vapor ?ux were signi?cantly reduced when severe pollution occurred.
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