Summertime ozone sensitivity to temperature in China: observational evidence and mechanistic attribution in urban and rural areas in the Yangtze River Delta region

IF 5.7 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES
Chang Su,Massimo Bollasina,James Weber,David Stevenson
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Abstract

As climate change increases frequency and intensity of hot extremes, understanding how elevated temperatures influence surface ozone (O 3 ) across different chemical regimes is critical. We combine observations from summer 2022 in the Yangtze River Delta (YRD) with controlled United Kingdom Chemistry and Aerosols (UKCA) Box experiments for urban Shanghai and a lower-NO x , biogenically influenced Lishui regional environment. Observed daily-maximum O 3 increases with temperature at both sites, with a stronger response in Shanghai. Two-dimensional T -RH distributions show that O 3 rises with temperature and decreases with relative humidity (RH), implying that part of the temperature response is mediated by drying. Factorial box-model experiments separate the roles of temperature-driven shifts in chemical partitioning, diurnal thermal structure, temperature-dependent isoprene emissions, and humidity. In Shanghai, the increase in O 3 between 30 and 40 °C is dominated by BVOC-driven chemistry, with temperature-amplified isoprene emissions explaining most of the observed response. In Lishui, O 3 sensitivity is governed primarily by radical-NO x chemistry and thermal PAN-NO x cycling, with a much smaller role for BVOCs. Fixed RH scenarios substantially reduce the apparent contribution of “thermal chemistry”, highlighting humidity-dependent O x loss and HO x -NO x cycling as key modifiers of the climate penalty. Because the 0-D framework excludes transport and meteorological dynamics, the reported fractions isolate the local chemical and emission-driven component of the O 3 -temperature relationship. Within this scope, the results identify robust regime-specific mechanisms linking heat, humidity, precursor chemistry, and surface O 3 in the YRD and demonstrate the value of observation-constrained box models as a bridge to regional chemistry-climate simulations.
中国夏季臭氧对温度的敏感性:长江三角洲城乡地区的观测证据和机制归因
随着气候变化增加极端高温的频率和强度,了解温度升高如何影响不同化学制度下的地表臭氧(O 3)至关重要。我们将2022年夏季长江三角洲(YRD)的观测数据与英国化学和气溶胶(UKCA)箱(UKCA)在上海市区的对照试验和低nox生物影响的丽水区域环境相结合。观测到的日最大o3随气温升高而增加,其中上海的响应更强。二维T -RH分布表明,o3随温度升高而升高,随相对湿度(RH)降低,表明干燥介导了部分温度响应。析因箱模型实验分离了温度驱动的化学分配、日热结构、温度依赖的异戊二烯排放和湿度变化的作用。在上海,o3在30 ~ 40°C之间的增加主要是由bvoc驱动的化学反应,温度放大的异戊二烯排放解释了大部分观测到的响应。在丽水,o3的敏感性主要受自由基- no - x化学和热PAN-NO - x循环的控制,BVOCs的作用要小得多。固定的RH情景大大减少了“热化学”的明显贡献,突出了湿度依赖的O x损失和HO x -NO x循环是气候惩罚的关键修饰因子。由于0-D框架排除了运输和气象动力学,因此报告的部分分离了o3 -温度关系中局部化学和排放驱动的成分。在此范围内,研究结果确定了将长三角地区的热量、湿度、前体化学和表面臭氧联系起来的强大的特定机制,并证明了观测约束盒模式作为区域化学-气候模拟的桥梁的价值。
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来源期刊
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics 地学-气象与大气科学
CiteScore
10.70
自引率
20.60%
发文量
702
审稿时长
6 months
期刊介绍: Atmospheric Chemistry and Physics (ACP) is a not-for-profit international scientific journal dedicated to the publication and public discussion of high-quality studies investigating the Earth''s atmosphere and the underlying chemical and physical processes. It covers the altitude range from the land and ocean surface up to the turbopause, including the troposphere, stratosphere, and mesosphere. The main subject areas comprise atmospheric modelling, field measurements, remote sensing, and laboratory studies of gases, aerosols, clouds and precipitation, isotopes, radiation, dynamics, biosphere interactions, and hydrosphere interactions. The journal scope is focused on studies with general implications for atmospheric science rather than investigations that are primarily of local or technical interest.
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