主办单位:中国气象局沈阳大气环境研究所
国际刊号:ISSN 1673-503X
国内刊号:CN 21-1531/P

Journal of Meteorology and Environment ›› 2021, Vol. 37 ›› Issue (2): 56-63.doi: 10.3969/j.issn.1673-503X.2021.02.008

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Causes of a haze pollution event in Changchun in January of 2019

Jie YU1,2(),Yu-peng LI1,2,Li-xin SU1,2,Qi-duo SHAO1,2,Shang-feng LI1,2,Li DING1,2,Zong-ting GAO1,2,Lin-chang AN3   

  1. 1. Jilin Institute of Meteorological Science, Changchun 130062, China
    2. Jilin Provincial key Laboratory of Changbai Mountain & Climate Change, Changchun 130062, China
    3. National Meteorological Center, Beijing 100081, China
  • Received:2020-04-27 Online:2021-04-01 Published:2021-04-02

Abstract:

Using air quality monitoring data, surface meteorological data, and LiDAR detection data, we analyzed the variation of air pollutants and meteorological parameters and the influence mechanisms during a haze pollution event in Changchun during January 10-15, 2019.The results showed that the heaviest pollution period occurs on January 12-13, with mass concentrations of PM2.5 and PM10 exceeding 150 μg·m-3 and the aerosol extinction coefficient reaching the highest level.The PM2.5/PM10 ratio values are higher than 0.7 at most times (>70%), indicating the important contribution of fine particles to this heavy pollution event.During heavy pollution period, near-surface wind speed remains low, relative humidity increases, air pressure varies hardly, and low-level wind direction changes.Weak descending motion, temperature inversion, and shallow boundary layer weaken the horizontal and vertical diffusion capacity of the atmosphere together, which favors the accumulation of air pollutants and the formation of this haze pollution.Changchun is located ahead of a trough and in the rear of a ridge at 500 hPa.Meanwhile, weak westerly winds prevail and relative humidity is high at 850 hPa.The sea-surface air pressure field is characterized by low-pressure cyclones and weak southwest flows, which results in the transport of pollutants to Changchun and enhances haze pollution.On January 14-15, the upper-level trough is deepened and moves eastwards, and the northwest airflow at 850 hPa and the near-surface pressure gradient are strengthened, leading to the dispersion of air pollutants and ending this haze pollution event.

Key words: Haze pollution, Meteorological condition, Aerosol extinction coefficient

CLC Number: