GSTDTAP  > 地球科学
DOI10.5194/acp-20-3191-2020
The long-term trend and production sensitivity change in the US ozone pollution from observations and model simulations
He, Hao1,2; Liang, Xin-Zhong1,2; Sun, Chao1; Tao, Zhining3,4; Tong, Daniel Q.1,5
2020-03-17
发表期刊ATMOSPHERIC CHEMISTRY AND PHYSICS
ISSN1680-7316
EISSN1680-7324
出版年2020
卷号20期号:5页码:3191-3208
文章类型Article
语种英语
国家USA
英文摘要

We investigated the ozone pollution trend and its sensitivity to key precursors from 1990 to 2015 in the United States using long-term EPA Air Quality System (AQS) observations and mesoscale simulations. The modeling system, a coupled regional climate-air quality model (CWRF-CMAQ; Climate-Weather Research Forecast and the Community Multiscale Air Quality), captured well the summer surface ozone pollution during the past decades, having a mean slope of linear regression with AQS observations of similar to 0.75. While the AQS network has limited spatial coverage and measures only a few key chemical species, CWRF-CMAQ provides comprehensive simulations to enable a more rigorous study of the change in ozone pollution and chemical sensitivity. Analysis of seasonal variations and diurnal cycle of ozone observations showed that peak ozone concentrations in the summer afternoon decreased ubiquitously across the United States, up to 0.5 ppbv yr(-1) in major non-attainment areas such as Los Angeles, while concentrations at certain hours such as the early morning and late afternoon increased slightly. Consistent with the AQS observations, CMAQ simulated a similar decreasing trend of peak ozone concentrations in the afternoon, up to 0.4 ppbv yr(-1), and increasing ozone trends in the early morning and late afternoon. A monotonically decreasing trend (up to 0.5 ppbv yr(-1)) in the odd oxygen (O-x=O-3 + NO2) concentrations are simulated by CMAQ at all daytime hours. This result suggests that the increased ozone in the early morning and late afternoon was likely caused by reduced NO-O-3 titration, driven by continuous anthropogenic NOx emission reductions in the past decades. Furthermore, the CMAQ simulations revealed a shift in chemical regimes of ozone photochemical production. From 1990 to 2015, surface ozone production in some metropolitan areas, such as Baltimore, has transited from a VOC-sensitive environment (> 50% probability) to a NOx-sensitive regime. Our results demonstrated that the long-term CWRF-CMAQ simulations can provide detailed information of the ozone chemistry evolution under a changing climate and may partially explain the US ozone pollution responses to regional and national regulations.


领域地球科学
收录类别SCI-E
WOS记录号WOS:000521140400002
WOS关键词RADICAL PROPAGATION EFFICIENCY ; NOX-HYDROCARBON SENSITIVITY ; NORTHEASTERN UNITED-STATES ; SURFACE OZONE ; AIR-QUALITY ; TROPOSPHERIC OZONE ; REGIONAL CLIMATE ; INDICATORS ; EMISSIONS ; IMPACTS
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/278690
专题地球科学
作者单位1.Univ Maryland, Dept Atmospher & Ocean Sci, College Pk, MD 20742 USA;
2.Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20742 USA;
3.Univ Space Res Assoc, Columbia, MD 21046 USA;
4.NASA, Goddard Space Flight Ctr, Code 916, Greenbelt, MD 20771 USA;
5.George Mason Univ, Ctr Spatial Informat Sci & Syst, Fairfax, VA 22030 USA
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GB/T 7714
He, Hao,Liang, Xin-Zhong,Sun, Chao,et al. The long-term trend and production sensitivity change in the US ozone pollution from observations and model simulations[J]. ATMOSPHERIC CHEMISTRY AND PHYSICS,2020,20(5):3191-3208.
APA He, Hao,Liang, Xin-Zhong,Sun, Chao,Tao, Zhining,&Tong, Daniel Q..(2020).The long-term trend and production sensitivity change in the US ozone pollution from observations and model simulations.ATMOSPHERIC CHEMISTRY AND PHYSICS,20(5),3191-3208.
MLA He, Hao,et al."The long-term trend and production sensitivity change in the US ozone pollution from observations and model simulations".ATMOSPHERIC CHEMISTRY AND PHYSICS 20.5(2020):3191-3208.
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