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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Regional and local background ozone in Houston during Texas AirQuality Study 2006
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Regional and local background ozone in Houston during Texas AirQuality Study 2006

机译:地区和地方背景臭氧在休斯顿2006年在德州AirQuality研究

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摘要

Principal Component Analysis (PCA) is used to isolate the common modes ofbehavior in the daily maximum 8-h average ozone mixing ratios measured at 30Continuous Ambient Monitoring Stations in the Houston-Galveston-Brazoria areaduring the Second Texas Air Quality Study field intensive (1 August to 15 October 2006).Three principal components suffice to explain 93% of the total variance. Nearly 84%is explained by the first component, which is attributed to changes in the "regionalbackground" determined primarily by the large-scale winds. The second component (6%)is attributed to changes in the "local background," that is, ozone photochemicallyproduced in the Houston area and spatially and temporally averaged by local circulations.Finally, the third component (3.5%) is attributed to short-lived plumes containing highozone originating from industrial areas along Galveston Bay and the Houston ShipChannel. Regional background ozone concentrations derived using the first componentcompare well with mean ozone concentrations measured above the Gulf of Mexico by thetunable profiler for aerosols and ozone lidar aboard the NOAA Twin Otter. The PCAregional background values also agree well with background values derived using thelowest daily 8-h maximum method of Nielsen-Gammon et al. (2005), provided theGalveston Airport data (C34) are omitted from that analysis. The differences found whenGalveston is included are caused by the sea breeze, which depresses ozone at Galvestonrelative to sites further inland. PCA removes the effects of this and other local circulationsto obtain a regional background value representative of the greater Houston area.
机译:主成分分析(PCA)是用来分离的常见模式ofbehavior日报最大8小时平均臭氧混合比率来衡量30岁时连续环境监测站的Houston-Galveston-Brazoria areaduring的第二个德克萨斯州空气质量研究领域集中(12006年8月到10月15日)。组件足以解释总数的93%方差。组件,它是由于变化“regionalbackground”主要由决定大规模的风。变化归因于“当地背景”,臭氧photochemicallyproduced在休斯顿和时空上由当地发行量平均。组件(3.5%)是短暂的包含highozone来自羽毛加尔维斯顿湾沿岸和工业区域休斯顿ShipChannel。使用第一个浓度派生componentcompare意味着臭氧浓度测量以上墨西哥湾thetunable分析器的气溶胶和臭氧激光雷达在NOAA双水獭。背景值与背景也同意值导出使用thelowest每日8小时最大尼尔森·盖蒙et al .(2005)的方法theGalveston机场数据(C34)被省略了这种分析。包括whenGalveston是由大海微风,抑制了臭氧Galvestonrelative网站进一步的内陆。删除这和其他地方的影响circulationsto获得区域背景值大休斯顿地区的代表。

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