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Impacts of Background Ozone Production on Houston and Dallas, Texas, Air Quality During the Second Texas Air Quality Study Field Mission

机译:在第二次德克萨斯州空气质量研究实地考察期间,背景臭氧生产对德克萨斯州休斯顿和达拉斯空气质量的影响

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摘要

A major objective of the 2006 Second Texas Air Quality Study (TexAQS II) focused on understanding the effects of regional processes on Houston and Dallas ozone nonattainment areas. Here we quantify the contributions of background (continental scale) ozone production on Houston and Dallas air quality during TexAQS II using ensemble Lagrangian trajectories to identify remote source regions that impact Houston and Dallas background ozone distributions. Global-scale chemical analyses, constrained with composition measurements from instruments on the NASA Aura satellite, are used to provide estimates of background composition along ensemble back trajectories. Lagrangian averaged O-3 net photochemical production (production minus loss, P-L) rates along the back trajectories are used as a metric to classify back trajectories. Results show that the majority (6 out of 9 or 66%) of the periods of high ozone in Houston were associated with periods of enhanced background ozone production. Slightly less than 50% (7 out of 15) of the days with high ozone in the Dallas Metropolitan Statistical Area (MSA) show enhanced background ozone production. Source apportionment studies show that 5-day Lagrangian averaged O-3 P-L in excess of 15 ppbv/d can occur during continental-scale transport to Houston owing to NOy enhancements from emissions within the Southern Great Lakes as well as recirculation of the Houston emissions. Dallas background O-3 P-L is associated with NOy enhancements from emissions within Chicago and Houston.
机译:2006年第二次德克萨斯州空气质量研究(TexAQS II)的主要目标集中在了解区域性过程对休斯顿和达拉斯臭氧不达标地区的影响。在这里,我们使用集合拉格朗日轨迹来量化TexAQS II期间背景(大陆尺度)臭氧生产对休斯敦和达拉斯空气质量的贡献,以识别影响休斯顿和达拉斯背景臭氧分布的偏远源区。全球规模的化学分析,再加上来自NASA Aura卫星上仪器的成分测量,被用来提供沿集合后向轨迹的背景成分的估计。拉格朗日沿后向轨迹的平均O-3净光化学净产量(产量减去损失,P-L)比率用作对后向轨迹进行分类的度量。结果显示,休斯顿的大部分高臭氧时期(9个中的6个,即66%)与背景臭氧产生增加的时期有关。达拉斯都市统计区(MSA)中臭氧含量高的日子中,不到50%的日子(15之7)显示出背景臭氧的产生增加。来源分配研究表明,由于南部大湖内排放物的NOy增强以及休斯敦排放物的再循环,在向休斯敦进行大陆规模运输期间,五日拉格朗日平均O-3 P-L可能超过15 ppbv / d。达拉斯的O-3 P-L背景与芝加哥和休斯顿的NOy排放增加有关。

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