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<article xsi:noNamespaceSchemaLocation="http://jats.nlm.nih.gov/publishing/1.1/xsd/JATS-journalpublishing1-mathml3.xsd" dtd-version="1.1" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"><front><journal-meta><journal-id journal-id-type="publisher-id">TACS</journal-id><journal-title-group><journal-title>Technology and Application of Computer Science</journal-title></journal-title-group><issn>2998-8926</issn><eissn>2998-8934</eissn><publisher><publisher-name>Art and Technology</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.61369/TACS.2025140047</article-id><article-categories><subj-group subj-group-type="heading"><subject>Article</subject></subj-group></article-categories><title>温度对臭氧浓度影响的研究综述</title><url>https://artdesignp.com/journal/TACS/2/14/10.61369/TACS.2025140047</url><author>彭婷婷</author><pub-date pub-type="publication-year"><year>2025</year></pub-date><volume>2</volume><issue>14</issue><history><date date-type="pub"><published-time>2025-07-28</published-time></date></history><abstract>近地面臭氧（O3）是重要的二次大气污染物，其对人体健康、生态系统和气候变化具有显著影响。温度作为影响臭氧生成的关键气象因子，通过调控光化学反应速率、前体物排放强度及气象条件影响臭氧浓度的时空分布。本文基于近年来的国内外研究文献，系统梳理温度对臭氧浓度的影响机制、极端天气事件的作用及未来气候情景下的变化趋势。研究发现，温度通过加速光化学反应、增强生物源和人为源挥发性有机物（VOCs）排放、改变大气边界层结构和区域输送条件等途径影响臭氧浓度；热浪等极端高温事件可导致臭氧浓度急剧上升，形成&amp;ldquo;气候惩罚&amp;rdquo;效应；未来气候变暖将加剧臭氧污染，部分抵消减排措施的成效。本文旨在为臭氧污染防控和气候适应政策提供科学依据。</abstract><keywords>臭氧,温度,挥发性有机物,光化学反应,热浪</keywords></article-meta></front><body/><back><ref-list><ref id="B1" content-type="article"><label>1</label><element-citation publication-type="journal"><p>[1]Fiore A. M., V. Naik, D. V. Spracklen, et al. Global air quality and climate [J]. Chemical Society Reviews, 2012, 41(19): 6663-83.[2]Lu X., L. Zhang, Y. Chen, et al. Exploring 2016-2017 surface ozone pollution over China: source contributions and meteorological influences [J]. Atmospheric Chemistry and Physics, 2019, 19(12): 8339-61.[3]Wang X., S. Yin, R. Zhang, et al. Assessment of summertime O3 formation and the O3-NOx-VOC sensitivity in Zhengzhou, China using an observation-based model [J]. Science of The Total Environment, 2022, 813: 152449.[4]Berg F., A. Novelli, R. Dubus, et al. Temperature-dependent rate coefficients for the reactions of OH radicals with selected alkanes, aromatic compounds, and monoterpenes [J]. Atmospheric Chemistry and Physics, 2024, 24(23): 13715-31.[5]Calfapietra C., S. Fares, F. Lofeto. Volatile organic compounds from Italian vegetation and their interaction with ozone [J]. Environmental Pollution, 2009, 157(5): 1478-86.[6]Rinnan R., L. L. Iversen, J. Tang, et al. Separating direct and indirect effects of rising temperatures on biogenic volatile emissions in the Arctic [J]. Proceedings of the National Academy of Sciences, 2020, 117(51): 32476-83.[7]Wu W., T.-M. Fu, S. R. Arnold, et al. Temperature-Dependent Evaporative Anthropogenic VOC Emissions Significantly Exacerbate Regional Ozone Pollution [J]. Environmental Science &amp;amp; Technology, 2024, 58(12): 5430-41.[8]Ryu Y.-H., J.-J. Baik, S.-H. Lee. Effects of anthropogenic heat on ozone air quality in a megacity [J]. Atmospheric Environment, 2013, 80: 20-30.[9]Steiner A. L. The influence of atmospheric chemistry and climate on atmosphere -biosphere interactions [M]. 2003.[10]Fu T.-M., H. Tian. Climate Change Penalty to Ozone Air Quality: Review of Current Understandings and Knowledge Gaps [J]. Current Pollution Reports, 2019, 5(3): 159-71.[11]Rasmussen D. M. The ozone-climate penalty: past, present and future [M]. 2013.[12]Bhattarai H., A. P. K. Tai, M. V. Martin, et al. Impacts of changes in climate, land use, and emissions on global ozone air quality by mid-21st century following selected Shared Socioeconomic Pathways [J]. Science of the Total Environment, 2024, 906.[13]Garzon Ruiz A. Atmospheric Reactivity of Alcohols, Thiols and Fluoroalcohols With Chlorine Atoms [M]. 2007.[14]Wang H., K. Wu, Y. Liu, et al. Role of Heat Wave-Induced Biogenic VOC Enhancements in Persistent Ozone Episodes Formation in Pearl River Delta [J]. Journal of Geophysical Research-Atmospheres, 2021, 126(12).[15]Ryan R. G., E. A. Marais, E. Gershenson-Smith, et al. Measurement report: MAX-DOAS measurements characterise Central London ozone pollution episodes during 2022 heatwaves [J]. Atmospheric Chemistry and Physics, 2023, 23(12): 7121-39.[16]Carey P. E. Experimental and theoretical determination of the temperature dependent rate constant for the reaction of hydroxyl radicals with some volatile organic compounds [M]. 2015.
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