中國對流層NOx垂直柱總量分布特征及其與閃電活動的相關性分析
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國家自然科學基金青年科學基金項目(41305015),中國氣象科學研究院災害天氣國家重點實驗室開放課題(2017LASWB06)資助


Distribution of Tropospheric NOx Vertical Column Density in China and Its Correlation with Lightning Activity
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    摘要:

    閃電放電過程發出很強的光輻射,促進了光化學反應的進行,加快了NOx向上的垂直輸送,造成對流層上部NOx的增加。閃電生成氮氧化物(LNOx)是對流層上部NOx(NO和NO2)的主要來源,影響了對流層和平流層大氣成分的垂直分布。本文利用2005—2013年TRMM衛星LIS傳感器閃電密度和Aura衛星OMI傳感器對流層NO2垂直柱總量遙感觀測數據,分析了中國地區對流層NO2柱總量時空分布特征及其與閃電活動的相關性。發現,青藏高原地區對流層NO2柱總量與閃電密度變化特征一致,表現為夏季高,冬季低,該地區LNOx估算值約為 339 mol/次?;贚NOx估算值分析中國不同地區LNOx/NOx百分比分布特征,發現,青藏高原地區春季和夏季LNOx/NOx較高,約為20%~60%,秋季和冬季低于20%;與之相比,NOx排放較為嚴重的四川盆地、長江三角洲和珠江三角洲等地區普遍低于20%,中國地區LNOx/NOx百分比平均值低于10%。由此得出結論,LNOx是青藏高原地區NOx的主要排放源,人口密集和工業程度較高的四川盆地、長江三角洲和珠江三角洲地區NOx主要來自于其它排放源。研究結果揭示了中國地區對流層NOx柱總量分布特征及其與閃電活動的關系,對于研究閃電過程對于氮氧化物生成量的影響有重要意義。

    Abstract:

    Lightninggenerated NOx (LNOx) affects the distribution of atmospheric components and is the main source of Nitrogen Oxides (NOx) in the upper troposphere. Strong optical radiation produced by lightning discharge can induce photochemical reaction. Lightning discharge promotes the vertical transportation of NOx, which causes the increases of NOx content in the upper troposphere. This study is to make the quantitative analysis of the vertical column density distribution of tropospheric NOx in China and its correlation with lightning activity, by using the measurements of the lightning density observed by the LIS sensor equipped on TRMM satellite and the vertical column density of tropospheric NO2 observed by the OMI sensor equipped on Aura satellite from 2005 to 2013 respectively. It is found that the monthly variations of lightning density and tropospheric NO2 vertical column density are almost the same on the Tibet Plateau. Both of the lightning density and the tropospheric NO2vertical column density are high in summer and low in winder on the Tibet Plateau. The tropospheric NO2 vertical column density generated by each flash is about 339 mol/flash, which is evaluated by using the data from the Tibet Plateau. Based on the result of the lightninggenerated NOx, the temporal and spatial distributions of LNOx/NOx in China are evaluated. It is found that LNOx/NOx on the Tibet Plateau is about 20% to 50% in spring and summer and less than 20% in winter. The LNOx/NOx in Sichuan Basin, Yangtze River Delta and Pearl River Delta regions is high in summer and low in winter, and generally less than 20%. The average of LNOx/NOx in China is less than 10%. The lightninggenerated NOx is the main source of NOx on the Tibet Plateau, but is not the main source of NOx in Sichuan Basin, Yangtze River Delta, and Pearl River Delta regions. The results reveal the relationship between lightning activity and NOx distribution in the troposphere over China. It is also important for understanding tropospheric NOx vertical column density and its correlation with the lightning activity.

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曹冬杰,閆歡歡,齊瑾.中國對流層NOx垂直柱總量分布特征及其與閃電活動的相關性分析[J].氣象科技,2018,46(2):374~381

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  • 收稿日期:2017-03-23
  • 定稿日期:2017-10-20
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  • 在線發布日期: 2018-05-02
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