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袁东敏, 马小会. 2016年12月16~21日重度霾过程及大气环流异常[J]. 气候与环境研究, 2017, 22(6): 757-764. DOI: 10.3878/j.issn.1006-9585.2017.17029
引用本文: 袁东敏, 马小会. 2016年12月16~21日重度霾过程及大气环流异常[J]. 气候与环境研究, 2017, 22(6): 757-764. DOI: 10.3878/j.issn.1006-9585.2017.17029
Dongmin YUAN, Xiaohui MA. The Severe Haze Process in 16-21 December 2016 and Associated Atmospheric Circulation Anomalies[J]. Climatic and Environmental Research, 2017, 22(6): 757-764. DOI: 10.3878/j.issn.1006-9585.2017.17029
Citation: Dongmin YUAN, Xiaohui MA. The Severe Haze Process in 16-21 December 2016 and Associated Atmospheric Circulation Anomalies[J]. Climatic and Environmental Research, 2017, 22(6): 757-764. DOI: 10.3878/j.issn.1006-9585.2017.17029

2016年12月16~21日重度霾过程及大气环流异常

The Severe Haze Process in 16-21 December 2016 and Associated Atmospheric Circulation Anomalies

  • 摘要: 针对2016年12月16~21日华北黄淮及周边地区的重度霾过程开展了诊断分析,发现全球、区域大气环流异常和局地气象条件是此次重度霾形成的重要原因之一。在此次过程中,受重度霾影响的面积为71×104 km2,霾持续时间达到6 d,过程最高小时细颗粒物(PM2.5)浓度超过1100 μg/m3。东大西洋/西俄罗斯和西太平洋波列(中高层)和北极涛动(近地面)均表现为显著的正位相型分布,综合调控了华北黄淮局地的环流场和气象条件,有利于霾的发生。华北、黄淮上空的异常反气旋能够有效抑制垂直运动,减弱水平风速。与之对应,近地面层为明显的弱低压区和偏南暖湿气流。从局地气象条件看,地面小风速、高湿度以及浅薄的边界层是促使本次重度霾发生的重要因子。

     

    Abstract: The severe haze occurred over North China and Huanghuai area in 16-21 December 2016 was analyzed and the atmospheric circulation anomalies were diagnosed to reveal one of the important causes. The coverage of this severe haze was 71×104 km2, and the duration was six days. The highest measured hourly PM2.5 concentration was above 1100 μg/m3. The East Atlantic/West Russia and West Pacific teleconnections (mid-upper level) and Arctic Oscillation (near surface) were in their positive phases and affected local atmospheric circulations and meteorological conditions, which were favorable for the occurrence of haze. The anti-cyclone over North China and Huanghuai area effectively confined the vertical motion and weakened the surface wind speed. Meanwhile, there existed an obvious weak low pressure system near the surface with warm and humid southerly winds. From the perspective of local meteorological conditions, the weak surface wind and high humidity condition as well as the shallow boundary layer were most important contributors to the occurrence of the severe haze in 16-21 December 2016.

     

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