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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Analysis of the origin of the distribution of CO in the subtropical southern Indian Ocean in 2007
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Analysis of the origin of the distribution of CO in the subtropical southern Indian Ocean in 2007

机译:2007年南印度洋亚热带CO分布的起源分析。

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We show carbon monoxide (CO) distributions at different vertical levels over the subtropical southern Indian Ocean, analyzing an observation campaign using Fourier transform infrared (FTIR) solar absorption spectrometry performed in 2007 at Reunion Island (21°S, 55°E). The CO pollution levels detected by the FTIR measurements during the campaign show a doubling of the CO total columns during the Southern Hemisphere biomass burning season. Using correlative data from the Measurement of Pollution in the Troposphere instrument and back trajectories analyses, we show that the potential primary sources for CO throughout the troposphere in 2007 are southern Africa (June–August) and South America (September–October). A secondary potential contribution from Southeast Asia and Indonesia-Malaysia was identified in the upper troposphere, especially in July and September. We examine the relation between the Asian monsoon anticyclone seasonal cycle and this result. We also investigate the relative contribution of different areas across the globe to the CO concentration in the subtropical southern Indian Ocean in 2007 using backward simulations combining the Lagrangian model FLEXPART 6.2, the Global Fire Emissions Database (GFEDv2.1) and the Emission Database for Global Atmospheric Research (EDGARv3.2-FT2000). We confirm the predominance of the African and South American contributions in the CO concentration in the southern subtropical Indian Ocean below 11 km. We show that CO transported from Australia makes only a small contribution to the total CO concentration observed over Reunion Island, and that the long-range transport of CO coming from Southeast Asia and Indonesia-Malaysia is important, especially from June until September in the upper troposphere.
机译:我们显示了在亚热带南部印度洋不同垂直水平上的一氧化碳(CO)分布,并使用2007年在留尼汪岛(21°S,55°E)进行的傅里叶变换红外(FTIR)太阳吸收光谱分析了一项观测活动。在运动期间通过FTIR测量检测到的CO污染水平表明,在南半球生物质燃烧季节,CO总柱数增加了一倍。利用对流层仪器中污染测量的相关数据和反向轨迹分析,我们表明,2007年整个对流层中一氧化碳的潜在主要来源是南部非洲(6月至8月)和南美(9月至10月)。在对流层高层,特别是在7月和9月,确定了东南亚和印度尼西亚-马来西亚的次要潜在贡献。我们研究了亚洲季风反气旋季节周期与这一结果之间的关系。我们还使用结合拉格朗日模型FLEXPART 6.2,全球火灾排放数据库(GFEDv2.1)和全球排放数据库的反向模拟研究了2007年印度南部亚热带地区不同地区对CO浓度的相对贡献大气研究(EDGARv3.2-FT2000)。我们确认非洲和南美在11 km以下的南亚热带印度洋的CO浓度中占主要地位。我们表明,从澳大利亚运来的一氧化碳对留尼汪岛上观测到的一氧化碳总浓度的贡献很小,并且从东南亚和印度尼西亚-马来西亚的一氧化碳的远距离运输非常重要,尤其是从上半年的6月到9月。对流层。

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