Severe haze events in the Indo-Gangetic Plain during post-monsoon: Synergetic effect of synoptic meteorology and crop residue burning emission

被引:0
|
作者
Kumari, Sonal [1 ]
Verma, Nidhi [1 ]
Lakhani, Anita [1 ]
Kumari, K. Maharaj [1 ]
机构
[1] Dayalbagh Educ Inst, Dept Chem, Fac Sci, Agra 282110, Uttar Pradesh, India
关键词
Particulate matter; Ozone; Ions; AQI; Backward trajectory; PSCF;
D O I
10.1016/j.scitotenv.2021.145479
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In recent years, the frequent occurrence of haze events in the Indo-Gangetic Plain (IGP) during crop residue burning period has caused a serious reduction in atmospheric visibility and deteriorated air quality. The present study is carried out to investigate the haze event observed in IGP in Nov 2017 using ground-based observations, satellite data and synoptic meteorology to understand the possible factors responsible for haze formation. PM2.5 (particulate matter with aerodynamic diameter <= 2.5 mu m) concentrations and Air Quality Index (AQI) at two sites (Agra and Delhi) situated in the central Indo-Gangetic Plain (CIGP) showed a sudden increase in PM2.5 concentrations and deteriorated air quality during 7-14 Nov. To monitor the variation of particulate matter (PM) in IGP, PM2.5 and PM10 (particulate matter with aerodynamic diameter <= 10 mu m) concentrations were monitored at 22 stations in 12 cities of IGP during 1-15 Nov which also showed an increase in PM concentrations during haze event (7-14 Nov). Crop residue burning activities in north-west Indo-Gangetic Plain (NW-IGP) were observed during haze event. Synoptic weather conditions of IGP identified using geopotential height and wind at 700 hPa showed high-pressure systems and low winds in IGP favoring stagnant conditions during haze event. A detailed analysis of the variation of pollutants and meteorology was carried out at Agra. Ozone (O-3), carbon monoxide (CO). sulphur dioxide (SO2) and nitrogen oxides (NOx) showed higher concentrations during haze event along with lower temperature, low wind speed and high relative humidity. Aerosol ionic composition showed a higher contribution (similar to 84%) of Cl-, NO3-, SO42- and NH4+ to total soluble ions suggesting secondary aero- sol formation during haze event. (C) 2021 Elsevier B.V. All rights reserved.
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页数:11
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