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2017年至2021年期间人为排放和气象因素对得克萨斯州圣安东尼奥市春季臭氧差异的影响。

Impacts of anthropogenic emissions and meteorology on spring ozone differences in San Antonio, Texas between 2017 and 2021.

作者信息

Liu Xueying, Wang Yuxuan, Wasti Shailaja, Lee Tabitha, Li Wei, Zhou Shan, Flynn James, Sheesley Rebecca J, Usenko Sascha, Liu Fei

机构信息

Department of Earth and Atmospheric Sciences, University of Houston, Houston, TX, USA.

Department of Earth and Atmospheric Sciences, University of Houston, Houston, TX, USA.

出版信息

Sci Total Environ. 2024 Mar 1;914:169693. doi: 10.1016/j.scitotenv.2023.169693. Epub 2023 Dec 30.

Abstract

San Antonio has been designated as ozone nonattainment under the current National Ambient Air Quality Standards (NAAQS). Ozone events in the city typically occur in two peaks, characterized by a pronounced spring peak followed by a late summer peak. Despite higher ozone levels, the spring peak has received less attention than the summer peak. To address this research gap, we used the Weather Research and Forecasting (WRF)-driven GEOS-Chem (WRF-GC) model to simulate San Antonio's ozone changes in the spring month of May from 2017 to 2021 and quantified the respective contributions from changes in anthropogenic emissions and meteorology. In addition to modeling, observations from the San Antonio Field Studies (SAFS), the Texas Commission on Environmental Quality (TCEQ) Continuous Ambient Monitoring Stations (CAMS), and the spaceborne TROPOspheric Monitoring Instrument (TROPOMI) are used to examine and validate changes in ozone and precursors. Results show that the simulated daytime mean surface ozone in May 2021 is 3.8 ± 0.6 ppbv lower than in May 2017, which is slightly less than the observed average differences of -5.3 ppbv at CAMS sites. The model predicted that the anthropogenic emission-induced changes contribute to a 1.4 ± 0.5 ppbv reduction in daytime ozone levels, while the meteorology-induced changes account for a 2.4 ± 0.6 ppbv reduction over 2017-2021. This suggests that meteorology plays a relatively more important role than anthropogenic emissions in explaining the spring ozone differences between the two years. We additionally identified (1) reduced NO and HCHO concentrations as chemical reasons, and (2) lower temperature, higher humidity, increased wind speed, and a stronger Bermuda High as meteorological reasons for lower ozone levels in 2021 compared to 2017. The quantification of the different roles of meteorology and ozone precursor concentrations helps understand the cause and variation of ozone changes in San Antonio over recent years.

摘要

根据现行的国家环境空气质量标准(NAAQS),圣安东尼奥已被指定为臭氧未达标地区。该市的臭氧事件通常出现在两个高峰期,其特点是春季有一个明显的高峰,随后是夏末的高峰。尽管春季臭氧水平较高,但春季高峰受到的关注少于夏季高峰。为了填补这一研究空白,我们使用了由天气研究和预报(WRF)驱动的GEOS-Chem(WRF-GC)模型,来模拟2017年至2021年5月春季圣安东尼奥的臭氧变化,并量化了人为排放变化和气象因素各自的贡献。除了建模之外,还利用了圣安东尼奥实地研究(SAFS)、德克萨斯州环境质量委员会(TCEQ)的连续环境监测站(CAMS)以及星载对流层监测仪器(TROPOMI)的观测数据,来检验和验证臭氧及其前体的变化。结果表明,2021年5月模拟的白天平均地表臭氧比2017年低3.8±0.6 ppbv,略低于CAMS站点观测到的平均差异-5.3 ppbv。该模型预测,人为排放引起的变化导致白天臭氧水平降低1.4±0.5 ppbv,而气象因素引起的变化在2017 - 2021年期间导致臭氧水平降低2.4±0.6 ppbv。这表明,在解释这两年春季臭氧差异方面,气象因素比人为排放起着相对更重要的作用。我们还确定了:(1)NO和HCHO浓度降低是化学原因;(2)与2017年相比,2021年温度较低、湿度较高、风速增加以及百慕大高压增强是臭氧水平较低的气象原因。量化气象因素和臭氧前体浓度的不同作用,有助于了解近年来圣安东尼奥臭氧变化的原因和变化情况。

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