2006年春季沙塵天氣下背景地區大氣氣溶膠光學特性的觀測研究
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國家自然科學基金項目(40275006)和北京區域氣象科技創新基金項目(BRMCCJ200701)及國家重點基礎研究發展計劃(2006CB403703)共同資助


Observational Study of Aerosol Extinction Property during Dust Weather in Background Area
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    摘要:

    利用2006年3~5月北京上甸子本底站氣溶膠細粒子(PM2.5)質量濃度、吸收和散射系數的連續觀測資料,對2006年春季上甸子本底站清潔、污染輸送及典型沙塵天氣下氣溶膠的消光特性進行了分析。結果顯示:①本底站在春季清潔情況下PM2.5質量濃度、吸收和散射系數的日均值水平分別為:10 μg/m3、 7 Mm-1和20 Mm-1左右,單散射反照率分布在0.71~0.78之間;此次觀測到的污染輸送過程中PM2.5質量濃度、吸收和散射系數平均值分別為:145 μg/m3、44.5 Mm-1、374.3 Mm-1,單散射反照率分布在0.84~0.94之間;沙塵影響期間,PM2.5質量濃度、吸收和散射系數以及單散射反照率的測量結果分布在248.2~424.1 μg/m3、10.8~44.7 Mm-1、225.4~392.5 Mm-1和0.89~0.96之間。②觀測得出,沙塵影響集中的時段細粒子質量濃度、氣溶膠散射系數和氣溶膠吸收系數都成倍地上升,其中質量濃度和散射系數上升的幅度要高于吸收系數。③3種天氣條件的對比結果顯示,受沙塵天氣影響PM2.5質量濃度明顯上升,且逐時波動幅度大;吸收系數遠高于清潔天氣下的觀測結果,但比污染輸送過程的測量結果偏低;散射系數同樣高于清潔天氣下的觀測結果,與污染輸送情況下的測量結果接近。沙塵天氣導致顆粒物濃度明顯上升,其對氣溶膠粒子散射作用的貢獻要大于吸收作用。

    Abstract:

    Using the continuous data of PM2.5 mass concentration, aerosol absorbing and scattering coefficients collected during March and May 2006 at the Shangdianzi background station, a primary study of the optical properties of aerosol in sanddust weather is conducted. The results indicate: (1) In the selected clear days, the value of PM2.5 mass concentration and daily average absorbing and scattering coefficients were about 10 μg/m3, 7 Mm-1, 20 Mm-1, respectively. The value of singlescattering albedo ranged from 0.71 to 0.78. During the transportation of pollutants from urban area to the background station, the average PM2.5 mass concentration, absorbing and scattering coefficients were 145 μg/m3,445 Mm-1, and 374.3 Mm-1. The value of single scattering albedo ranged from 0.84 to 0.94.While in sanddust weather, the value of PM2.5 mass concentration, aerosol absorbing and scattering coefficients, single scattering albedo ranged from 248.2 μg/m3to 424.1 μg/m3, 10.8 Mm-1 to 44.7 Mm-1, 225.4 Mm-1 to 393.9 Mm-1, and 0.89 to 0.96, respectively. (2) Affected by the sanddust weather, the increasing ranges of aerosol mass concentration and scattering coefficients were much greater than that of absorbing coefficient. (3) Through comparing the results from the three kinds of weather, it is found that the sanddust weather made the concentration of particles increase up to an abnormally high value and fluctuate greatly in a short time. The absorbing coefficient of aerosol in sanddust weather was much higher than in clear days but lower than during the pollutant transporting process from urban area to background station. The scattering coefficient of aerosol in sanddust weather was much higher than in clear days, close to that during the pollution case. The sanddust weather contributed to the scattering effect more greatly than to the absorbing effect of aerosol.

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徐敬,張小玲,顏鵬,丁國安,徐曉峰.2006年春季沙塵天氣下背景地區大氣氣溶膠光學特性的觀測研究[J].氣象科技,2008,36(6):679~685

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  • 收稿日期:2008-01-17
  • 定稿日期:2008-03-26
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