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Ammonia emissions in tropical biomass burning regions: Comparison between satellite-derived emissions and bottom-up fire inventories

机译:热带生物质燃烧区的氨气排放:卫星排放与自下而上的火灾清单之间的比较

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摘要

Vegetation fires emit large amounts of nitrogen compounds in the atmosphere, including ammonia (NH3). These emissions are still subject to large uncertainties. In this study, we analyze time series of monthly NH3 total columns (molec cm(-2)) from the IASI sounder on board MetOp-A satellite and their relation with MODIS fire radiative power (MW) measurements. We derive monthly NH3 emissions estimates for four regions accounting for a major part of the total area affected by fires (two in Africa, one in central South America and one in Southeast Asia), using a simplified box model, and we compare them to the emissions from both the GFEDv3.1 and GFASv1.0 biomass burning emission inventories. In order to strengthen the analysis, we perform a similar comparison for carbon monoxide (CO), also measured by IASI and for which the emission factors used in the inventories to convert biomass burned to trace gas emissions are thought to be more reliable. In general, a good correspondence between NH3 and CO columns and the FRP is found, especially for regions in central South America with correlation coefficients of 0.82 and 0.66, respectively. The comparison with the two biomass burning emission inventories GFASv1.0 and GFEDv3.1 shows good agreements, particularly in the time of the maximum of emissions for the central South America region and in the magnitude for the region of Africa south of the equator. We find evidence of significant non-pyrogenic emissions for the regions of Africa north of the equator (for NH3) and Southeast Asia (for NH3 and CO). On a yearly basis, total emissions calculated from IASI measurements for the four regions reproduce fairly well the interannual variability from the GFEDv3.1 and GFASv1.0 emissions inventories for NH3 but show values about 1.5-2 times higher than emissions given by the two biomass burning emission inventories, even when assuming a fairly long lifetime of 36 h for that species. (C) 2015 Elsevier Ltd. All rights reserved.
机译:植被大火在大气中释放出大量的氮化合物,包括氨(NH3)。这些排放仍存在很大的不确定性。在这项研究中,我们分析了MetOp-A卫星上来自IASI测深仪的每月NH3总色谱柱的时间序列(molec cm(-2))及其与MODIS火辐射功率(MW)测量的关系。我们使用简化的箱型模型得出四个地区的每月NH3排放估算值,这些地区占火灾总面积的很大一部分(非洲两个,南美中部一个和东南亚一个),并将它们与GFEDv3.1和GFASv1.0生物质燃烧排放清单中的排放量。为了加强分析,我们对同样由IASI测量的一氧化碳(CO)进行了类似的比较,对于这些一氧化碳,库存中用于将燃烧的生物质转化为痕量气体排放的排放因子被认为更为可靠。通常,发现NH3和CO色谱柱与FRP之间具有良好的对应关系,尤其是在南美中部地区,相关系数分别为0.82和0.66。与两个生物质燃烧排放清单GFASv1.0和GFEDv3.1的比较显示出良好的协议,特别是在南美中部地区最大的排放时期和赤道以南的非洲地区的数量级。我们发现在赤道以北(对于NH3)和东南亚(对于NH3和CO)的非洲地区存在显着的非热原排放的证据。每年,根据IASI测量得出的四个地区的总排放量,可以很好地再现NH3的GFEDv3.1和GFASv1.0排放量清单的年际变化,但显示出的值比这两个生物质的排放量高1.5-2倍燃烧排放清单,即使假设该物种的寿命较长为36小时。 (C)2015 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Atmospheric environment》 |2015年第11期|42-54|共13页
  • 作者单位

    Univ Libre Bruxelles, Spect Atmosphere Chim Quant & Photophys, B-1050 Brussels, Belgium;

    Univ Libre Bruxelles, Spect Atmosphere Chim Quant & Photophys, B-1050 Brussels, Belgium|Vrije Univ Amsterdam, Fac Earth & Life Sci, Amsterdam, Netherlands;

    Max Planck Inst Chem, D-55128 Mainz, Germany;

    Vrije Univ Amsterdam, Fac Earth & Life Sci, Amsterdam, Netherlands;

    Univ Paris 06, Ecole Polytech, CNRS, INSU,LMD,IPSL, Palaiseau, France;

    Univ Libre Bruxelles, Spect Atmosphere Chim Quant & Photophys, B-1050 Brussels, Belgium;

    Univ Libre Bruxelles, Spect Atmosphere Chim Quant & Photophys, B-1050 Brussels, Belgium;

    Univ Libre Bruxelles, Spect Atmosphere Chim Quant & Photophys, B-1050 Brussels, Belgium|Univ Paris 06, Univ Versailles St Quentin, CNRS, INSU,LATMOS,IPSL, Palaiseau, France;

    Univ Libre Bruxelles, Spect Atmosphere Chim Quant & Photophys, B-1050 Brussels, Belgium;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Ammonia emissions; Vegetation fires; Fire radiative power; Biomass burning emission inventories; GFEDv3.1; GFASv1.0;

    机译:氨排放;植被火灾;火辐射功率;生物质燃烧排放清单;GFEDv3.1;GFASv1.0;

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