Chen Lin, Wang Lili, Ji Dongsheng, et al. Characteristics of atmospheric pollutants at Dinghushan Station during the Asian Games in Guangzhou. J Appl Meteor Sci, 2013, 24(2): 151-161.
Citation: Chen Lin, Wang Lili, Ji Dongsheng, et al. Characteristics of atmospheric pollutants at Dinghushan Station during the Asian Games in Guangzhou. J Appl Meteor Sci, 2013, 24(2): 151-161.

Characteristics of Atmospheric Pollutants at Dinghushan Station During the Asian Games in Guangzhou

  • Received Date: 2012-08-23
  • Rev Recd Date: 2012-12-14
  • Publish Date: 2013-04-30
  • To understand the air quality status and influences of meteorological factors on concentrations of regional background pollutants in Southern China, online measurements of nitrogen oxide, sulfur dioxide, ozone, PM10 and PM2.5 observations are conducted in Mount Dinghu Background Monitoring Station in November of 2010. MICAPS data, NCEP FNL data and HYSPLIT model are used to deeply analyze the relationship between synoptic circulation, divergence and vorticity, meteorological factors, pollutant source regions and variation characteristics of pollutants in different periods. The results show that the average concentrations of NO2, SO2 and O3 in Mount Dinghu area are (7.2±3.1)×10-9, (8.5±3.8)×10-9 and (28.7±9.8)×10-9, respectively, during the Asian Games period.The aerosol pollution in this region is serious, with the monthly average concentration of PM10 for 113 μg·m-3 and PM2.5 for 81 μg·m-3, and the daily average concentration of PM2.5 exceeds the WHO IT.1 air quality standard for 13 days. The analyses on air pollutants during high-level pollution periods show that the average concentrations of NOx and O3 are 13.2×10-9 and 20.9×10-9, which decreases by 41.3% and 10.7% than those in 2009, but the average concentration of SO2 hardly changes in 2010 compared with that in 2009. All the results suggest that the air quality control measure is effective in some degree. However, the concentrations of PM10 and PM2.5 during the period of the Asian Games are higher than those during the same period in 2009, due to relatively stable meteorological conditions, fine weather and high temperature, while the continuous precipitations leads to the lower values of PM10 and PM2.5 during the same period in 2009. High temperature and humidity caused by uniform pressure and temperature fields of the generation of high pressure, continued convergence, weak rising mechanism, the weak surface wind at the surface layer and regional transport lead to the accumulation of primary air pollutants and fine particles. Backward trajectory simulation results show that the flows, originating from east, lead an obvious increase in primary air pollutants, fine particles and atmospheric oxidation in the areas of Mount Dinghu, which pass the industrial areas in Pearl River Delta. In summary, higher concentrations of PM2.5 in Pearl River Delta regional background area are attributed to adverse meteorological condition and pollutant transport.
  • Fig. 1  Concentration variation of NOx, SO2, O3, PM in Nov 2010 (a) hourly average, (b) daily average

    Fig. 2  Pollutant average diurnal variation in low concentration period and high concentration period

    (the value within the brackets is average concentration for each pollutant)

    Fig. 3  Diurnal variation of meteorological factors and pollutant concentrations at Mout Dinghu in 2010(a)3 November to 5 November, (b)27 November to 28 November

    Fig. 4  Correlation analysis of [O3] and [NO2]/[NO] during low and high concentration periods at Mount Dinghu in 2010(a)3 November to 5 November, (b)27 November to 28 November

    Fig. 5  Height-time section of regional average diffusion (unit:10-5s-1) and vertical velocity (unit:Pa·s-1) at Mount Dinghu during 3—5 November and 27—28 November in 2010

    Fig. 6  24 h back-trajectory simulation for the air mass arrived at Mount Dinghu in different periods in November 2010

    Table  1  Typical high and low pollutant concentration processes and corresponding weather patterns

    典型过程 时段 对应天气形势 天气状况
    低值 2009-11-02—04 冷高压南下 多云
    2009-11-12—16 冷高脊 阴有中到大雨
    2009-11-18—19 冷高压南下 多云转阴
    2010-11-03—05 冷高压南下 晴转阴雨
    2010-11-15—16 冷高压南下
    2010-11-18—19 变性高压脊后部 多云
    2010-11-25—26 冷高压变性 晴间多云
    高值 2009-11-06—07 变性脊回流 多云转阴
    2009-11-26—27 变性高压脊 多云
    2010-11-23—24 变性高压脊
    2010-11-27—28 变性高压脊 多云
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    • Received : 2012-08-23
    • Accepted : 2012-12-14
    • Published : 2013-04-30

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