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Monitoring emissions from the 2015 Indonesian fires using CO satellite data

机译:使用CO卫星数据监控2015年印尼大火的排放

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摘要

Southeast Asia, in particular Indonesia, has periodically struggled with intense fire events. These events convert substantial amounts of carbon stored as peat to atmospheric carbon dioxide (CO2) and significantly affect atmospheric composition on a regional to global scale. During the recent 2015 El Niño event, peat fires led to strong enhancements of carbon monoxide (CO), an air pollutant and well-known tracer for biomass burning. These enhancements were clearly observed from space by the Infrared Atmospheric Sounding Interferometer (IASI) and the Measurements of Pollution in the Troposphere (MOPITT) instruments. We use these satellite observations to estimate CO fire emissions within an inverse modelling framework. We find that the derived CO emissions for each sub-region of Indonesia and Papua are substantially different from emission inventories, highlighting uncertainties in bottom-up estimates. CO fire emissions based on either MOPITT or IASI have a similar spatial pattern and evolution in time, and a 10% uncertainty based on a set of sensitivity tests we performed. Thus, CO satellite data have a high potential to complement existing operational fire emission estimates based on satellite observations of fire counts, fire radiative power and burned area, in better constraining fire occurrence and the associated conversion of peat carbon to atmospheric CO2. A total carbon release to the atmosphere of 0.35–0.60 Pg C can be estimated based on our results.This article is part of a discussion meeting issue ‘The impact of the 2015/2016 El Niño on the terrestrial tropical carbon cycle: patterns, mechanisms and implications'.
机译:东南亚,尤其是印度尼西亚,定期发生激烈的火灾。这些事件将作为泥炭存储的大量碳转化为大气二氧化碳(CO2),并在区域到全球范围内显着影响大气成分。在最近的2015年厄尔尼诺事件中,泥炭大火大大增强了一氧化碳(CO)的含量,这是一种空气污染物,是生物质燃烧的著名示踪剂。红外大气探测干涉仪(IASI)和对流层污染测量(MOPITT)仪器从太空中清楚地观察到了这些增强作用。我们使用这些卫星观测值在逆模型框架内估算CO火灾排放。我们发现,印度尼西亚和巴布亚每个子区域的推导CO排放量与排放量清单有很大不同,这突显了自下而上估算的不确定性。基于MOPITT或IASI的CO火灾排放具有相似的空间格局和时间演变,根据我们进行的一系列敏感性测试,不确定性为10%。因此,CO卫星数据具有很大的潜力,可根据对火势,火辐射功率和燃烧面积的卫星观测结果,对现有的运行火排放估算值进行补充,从而更好地限制火势的发生以及与之相关的泥炭向大气CO2的转化。根据我们的结果,可以估算出向大气中释放的总碳为0.35-0.60 PgC。本文是“ 2015/2016厄尔尼诺现象对陆地热带碳循环的影响:模式,机制”讨论会的一部分和影响”。

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