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2016冬季京津冀一次持续重度霾天气过程分析
引用本文:毛曳,张恒德,朱彬. 2016冬季京津冀一次持续重度霾天气过程分析[J]. 环境科学, 2021, 42(8): 3615-3621
作者姓名:毛曳  张恒德  朱彬
作者单位:南京信息工程大学大气物理学院,南京210044;国家气象中心,北京100081;气象灾害预报预警与评估协同创新中心,南京210044
基金项目:国家重点研发计划项目(2016YFC0203301)
摘    要:2016年12月16~21日我国京津冀地区发生了一次持续重度霾天气过程.为了进一步加深对霾的认识和提高对霾的分析预报能力,利用多种资料,对此次重度霾天气过程的环流背景和气象要素等进行了综合性分析.结果 表明,此次过程持续时间长,污染强度大,影响范围广,能见度低,以外来输送为主,气溶胶主要分布在600 m以下高度,有一定...

关 键 词:  环流背景  气象要素  激光雷达  极端性
收稿时间:2020-12-05
修稿时间:2021-01-17

Analysis of the Continuous Heavy Pollution Process in the Winter of 2016 in Beijing, Tianjin, and Hebei
MAO Ye,ZHANG Heng-de,ZHU Bin. Analysis of the Continuous Heavy Pollution Process in the Winter of 2016 in Beijing, Tianjin, and Hebei[J]. Chinese Journal of Environmental Science, 2021, 42(8): 3615-3621
Authors:MAO Ye  ZHANG Heng-de  ZHU Bin
Affiliation:School of Atmospheric Physics, Nanjing University of Information Science & Technology, Nanjing 210044, China;National Meteorological Centre, Beijing 100081, China; Collaborative Innovation Center for Meteorological Disaster Prediction and Assessment, Nanjing 210044, China
Abstract:From December 16 to 21, 2016, continuous heavy haze occurred in the Beijing-Tianjin-Hebei region of China. To further understand the development mechanism of haze and improve the forecasting of haze events, a variety of data, background circulation, and the meteorological elements of this severe haze process were comprehensively analyzed. The results show that the process lasted for a long time, pollution intensity was high, influence area was wide, visibility was low, and external transport was the main cause. Aerosols were mainly distributed at a height of 600 m, and there was a certain extreme anomaly. The static weather index and air quality index showed a strong correlation. The air in the Beijing-Tianjin-Hebei region is controlled by zonal circulation in front of a high-pressure ridge, which maintains the westerly airflow. Cold-air activity is weak, and downflow is dominant. The water vapor content is low, the cloud cover is limited at high altitudes, and a warm ridge extends northwards at low altitudes. Limited static wind on the ground, high relative humidity, and low mixing-layer height are not conducive to the horizontal and vertical diffusion of pollutants.
Keywords:haze  circulation background  meteorological elements  laser radar  extremity
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