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Ozone enhancement in western US wildfire plumes at the Mt. Bachelor Observatory: The role of NOx

机译:美国西部山野火烟囱的臭氧增强。学士天文台:NOx的作用

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摘要

We looked at 19 wildfire events that were observed in the summers of 2012 and 2013 at the Mt. Bachelor Observatory (MBO, 2.7 km a.s.l.), a mountaintop site located in central Oregon. We identified wildfire plumes using enhancement ratios (Delta Y/Delta X), which we calculated for each plume by taking the Reduced Major Axis linear regression slope of various species. We reported the calculated enhancement ratios and explored their relationship with ozone production. We observed a negative correlation between Delta O-3/Delta CO and Delta NOx/Delta NOy (r = -0.72). This showed that the degree of NOx oxidation is a key predictor of ozone production. The highest Delta NOx/Delta NOy (0.57 pptv/pptv) was associated with ozone loss (ozone titration). Low Delta NOx/Delta NOy values (ranging from 0.049 to 0.15 pptv/pptv) are generally associated with ozone enhancement. We also found that even if Delta O-3/Delta CO is low, Delta O-3 may still be significant if CO enhancements are large. We then explored events that are not associated with any O-3 enhancement/loss. Out of 19 fire events, 3 belong to this category. We discovered that these events are either BL-influenced (O-3 deposition), associated with low Delta NOy/Delta CO ratios, and/or associated with minimal photochemistry (due to nighttime transport). Absolute ozone enhancements ranged from 3.8 to 32 ppbv, while ozone production efficiencies (OPEs) ranged from 2.1 to 17. However, because PAN comprises most of the reactive nitrogen in fire plumes, the calculated OPEs underestimated the true ozone mixing ratios. OPEs may therefore be misleading indicators of ozone production in wildfires. Finally, we segregated the data into plumeon-plume time periods. From this we found that the average O-3 mixing ratio was significantly higher in fire plumes compared to non-plume time periods, and the noontime NO/NO2 ratios were also higher. This later result gives insight into the photochemical environment in the fire plumes. (C) 2014 Elsevier Ltd. All rights reserved.
机译:我们研究了2012年和2013年夏季在山峰观测到的19次野火事件。学士天文台(MBO,2.7公里a.s.l.),位于俄勒冈州中部的山顶。我们使用增强比(Delta Y / Delta X)来识别野火羽流,我们通过采用各种物种的减少的主轴线性回归斜率来计算每个羽流。我们报告了计算出的增强比,并探讨了它们与臭氧产生的关系。我们观察到Delta O-3 / Delta CO与Delta NOx / Delta NOy之间呈负相关(r = -0.72)。这表明NOx氧化程度是臭氧产生的关键预测指标。最高的Delta NOx / Delta NOy(0.57 pptv / pptv)与臭氧损失(臭氧滴定)有关。低Delta NOx / Delta NOy值(范围从0.049至0.15 pptv / pptv)通常与臭氧增强有关。我们还发现,即使Delta O-3 / Delta CO较低,但如果CO增强很大,Delta O-3可能仍然很重要。然后,我们探索了与任何O-3增强/损失都不相关的事件。在19起火灾中,有3个属于此类。我们发现这些事件受BL影响(O-3沉积),与低Delta NOy / Delta CO比有关,和/或与最小化光化学有关(由于夜间运输)。绝对臭氧增强范围为3.8至32 ppbv,而臭氧生产效率(OPE)为2.1至17。但是,由于PAN包含火羽中的大部分活性氮,因此计算得出的OPE低估了真实的臭氧混合比。因此,OPES可能会误导野火中臭氧产生的指标。最后,我们将数据分为羽状/非羽状时间段。从中我们发现,火羽中的平均O-3混合比与非泡沫时期相比显着更高,并且正午时的NO / NO2比也更高。以后的结果可以深入了解火羽中的光化学环境。 (C)2014 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Atmospheric environment》 |2015年第5期|297-304|共8页
  • 作者单位

    Univ Washington, Dept Atmospher Sci, Seattle, WA 98195 USA;

    Univ Washington, Dept Atmospher Sci, Seattle, WA 98195 USA|Univ Washington, Sch Sci & Technol, Bothell, WA 98011 USA;

    Univ Washington, Dept Atmospher Sci, Seattle, WA 98195 USA;

    Univ Washington, Sch Sci & Technol, Bothell, WA 98011 USA;

    Univ Washington, Sch Sci & Technol, Bothell, WA 98011 USA;

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

    Ozone production; Wildfire; Enhancement ratio; Western U.S;

    机译:臭氧生产;野火;增效率;美国西部;

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