綿陽城區一次連續重污染過程的氣象條件分析
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Weather Condition Analysis of a Urban Heavy Pollution Event
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    基于高密度逐時氣象觀測資料以及國家環境保護部公布的空氣質量日報,對綿陽城區2014年1月9日至2月4日一次污染過程的氣象條件,分3種類型(輕度污染型、中度污染型、重度污染型)進行研究。結果表明:整個過程風速和混合層厚度與空氣質量指數均呈負相關,相關系數為-0637、-0487;分類型討論時,僅輕度污染型風速與空氣質量指數呈負相關,相關系數為-0739;風速日變化均呈現“單峰型”的特征,峰值出現在12:00—18:00之間;風向以東南、西北氣流為主,東南氣流能加重空氣污染;混合層厚度表現為“早晚低,午后高”的日變化特征,輕度型的混合層厚度平均高58378 m,中度型反比重度型低6 m,分別為48192 m,48769 m;潰變理論V3θ圖對連續重污染過程的轉折性天氣起到較好的預報和指示作用,主要表現在強對流和降水天氣兩類。

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    Based on the hourly highdensity meteorological observation data and the Air Quality Index announced by the Ministry of Environmental Protection of China, we discuss and analyze the meteorological conditions of the pollution process from January 9 to 4 February 2014 in the urban area of Mianyang, Sichuan ProvinceThis study is conducted from three aspects: slight, moderate, and severe pollutionAnalysis indicates that the wind speed and the thickness of the atmospheric mixed layer are negatively correlated with the air quality index, with the correlation coefficients being -0637 and -0487The types of air pollution are discussedThe wind speed is negatively correlated with the air quality index in slight pollution with a correlation coefficient of -0739The diurnal variation of wind speed shows a singlepeak trend, with the peak value appearing in 12:00-18:00The wind direction is given priority to the southeast and northwest flow, and the air pollution could be aggravated by the southeast flowThe thickness of the atmospheric mixed layer in the slight pollution condition is 58378 m, and it is 5 m lower in moderate pollution than in severe pollution, 48192 m and 48769 m, respectively While the thickness of the atmospheric mixed layer on the low side, the diurnal variation is characterized as low in the morning and evening, high in the afternoon According to the Blownup Theory, the 〖WTBX〗V〖WTBZ〗3〖WTBX〗θ〖WTBZ〗 plot of the pollution process has instructive effect in forecasting strong convection and precipitation

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杜筱筱,馬力.綿陽城區一次連續重污染過程的氣象條件分析[J].氣象科技,2017,45(4):717~724

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  • 收稿日期:2016-05-18
  • 定稿日期:2017-04-28
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  • 在線發布日期: 2017-08-30
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