Abstract

Crop residue burning is one of the important types of biomass burning in China and has potentially important effect on air quality and climate. A coupled meteorology and aerosol/chemistry model (WRF-Chem) with ground and satellite observations and biomass burning emission inventory were applied to investigate the spatial/temporal distribution and transport pathways of air pollutants and to quantify the contribution of crop residue burning to aerosol concentration in the North China Plain, with focus on Beijing and Tianjin during a severe haze episode on 7–11 October 2014, when the daily mean surface PM2.5 concentration in Beijing reached 317 µg m–3. During this period, intensive crop fires were detected over wide areas of eastern Henan, southern Hebei and western Shandong, and the crop residue burning emission was much larger than anthropogenic emission in major fire areas. Model comparison with ground observations demonstrated the WRF-Chem was able to generally reproduce surface meteorological variables and PM2.5 concentration, although it tended to overpredict wind speed and aerosol concentration in some locations. Taking crop residue burning into account can apparently improve PM2.5 prediction during the haze episode. The stagnant weather condition favored haze formation and maintenance in this region, and crop residue burning intensified haze pollution in both fire source and downwind regions. The crop residue burning emission on average contributed 19% to surface PM2.5 concentration in Beijing during the haze episode, in which it contributed 40% and 29% to organic carbon aerosol and primary PM2.5, respectively, and less to black carbon aerosol (4.9%). The impact of crop residue burning in Tianjin was smaller than that in Beijing, with an average contribution of 7.4% due to different fire sources and transport pathways.

Highlights

  • Open biomass burning is one of the important sources of greenhouse gases, trace gases and particulate matter worldwide

  • Cheng et al (2013) developed a new source identification method which used levoglucosan to K+ ratio in combination with levoglucosan to mannosan ratio and confirmed that biomass burning aerosol in Beijing mainly came from the combustion of crop residuals, by using Positive Matrix Factorization (PMF) model they found about 50% of the organic carbon (OC) and EC in Beijing were associated with biomass burning during summer and winter of 2011

  • By applying the WRF-Chem model, FINN biomass burning emission inventory, ground and satellite observations, as well as back trajectory analysis, a severe haze event over the north China Plain during 7–11 October 2014 was investigated with focus on the impact of crop residue fire on surface PM2.5 concentrations in fire source and downwind areas and the transport pathways of fire emitted aerosols under typical weather condition

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Summary

Introduction

Open biomass burning is one of the important sources of greenhouse gases, trace gases and particulate matter worldwide. A coupled meteorology and aerosol/chemistry model (WRF-Chem) with ground and satellite observations and biomass burning emission inventory were applied to investigate the spatial/temporal distribution and transport pathways of air pollutants and to quantify the contribution of crop residue burning to aerosol concentration in the North China Plain, with focus on Beijing and Tianjin during a severe haze episode on 7–11 October 2014, when the daily mean surface PM2.5 concentration in Beijing reached 317 μg m–3.

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