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Identification of CO plumes from MOPITT data: Application to the August 2000 Idaho-Montana forest fires

机译:从mOpITT数据中识别CO羽流:应用于2000年8月的爱达荷 - 蒙大拿州森林火灾

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摘要

This study focuses on the identification of carbon monoxide ( CO) released during the forest fires that took place primarily in Montana and Idaho during the summer of 2000. We focus our analysis on the most intense period of the fires during the second half of August. During that period, the MOPITT instrument onboard the EOS-Terra platform collected extensive measurements of CO. A simulation of the dispersal of the CO from the fires, constrained by the AVHRR observations of fire location and extent, clearly identifies the affected regions. The model results are compared with the CO observations from the COBRA experiment flight on August 19. Using these various data, we are able to identify the transport of the CO plume originating from the fires. In particular, it is shown that the CO travels eastward from the fires, reaching as far as the East coast and the Gulf of Mexico in a few days. Although the distribution of CO over the U. S. is clearly a combination of a variety of sources it is found that wildfires are a strong component of the summer tropospheric CO.
机译:这项研究的重点是确定2000年夏季主要发生在蒙大拿州和爱达荷州的森林大火期间释放的一氧化碳(CO)。我们将分析重点放在8月下半月大火最强烈的时期。在此期间,EOS-Terra平台上的MOPITT仪器收集了广泛的CO测量值。通过AVHRR对火的位置和范围的观察加以限制,模拟了大火中CO的扩散,从而清楚地确定了受影响的区域。将模型结果与8月19日进行的COBRA实验飞行中的CO观测值进行比较。使用这些各种数据,我们能够确定源自火源的CO羽流的传输。尤其是,这表明一氧化碳从大火向东移动,几天之内就到达了东海岸和墨西哥湾。尽管一氧化碳在美国的分布显然是多种来源的结合,但发现野火是夏季对流层一氧化碳的重要组成部分。

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