State Key Laboratory of Severe Weather, Key Laboratory for Atmospheric Chemistry, Institute of Atmospheric Composition, Chinese Academy of Meteorological Sciences, Beijing, 100081, China; Department of Atmospheric and Oceanic Sciences, Fudan University, Shanghai, 200438, China.
Longfengshan Regional Atmosphere Background Station, China Meteorological Administration (CMA), Heilongjiang, 150200, China.
Environ Pollut. 2024 May 1;348:123748. doi: 10.1016/j.envpol.2024.123748. Epub 2024 Mar 7.
Surface ozone (O) is a crucial air pollutant that affects air quality, human health, agricultural production, and climate change. Studies on long-term O variations and their influencing factors are essential for understanding O pollution and its impact. Here, we conducted an analysis of long-term variations in O during 2006-2022 at the Longfengshan Regional Atmosphere Background Station (LFS; 44.44°N, 127.36°E, 330.5 m a.s.l.) situated on the northeastern edge of the Northeast China Plains. The maximum daily 8-h average (MDA8) O fluctuated substantially, with the annual MDA8 decreasing significantly during 2006-2015 (-0.62 ppb yr, p < 0.05), jumping during 2015-2016 and increasing clearly during 2020-2022. Step multiple linear regression models for MDA8 were obtained using meteorological variables, to decompose anthropogenic and meteorological contributions to O variations. Anthropogenic activities acted as the primary drivers of the long-term trends of MDA8 O, contributing 73% of annual MDA8 O variability, whereas meteorology played less important roles (27%). Elevated O at LFS were primarily associated with airflows originating from the North China Plain, Northeast China Plain, and coastal areas of North China, primarily occurring during the warm months (May-October). Based on satellite products of NO and HCHO columns, the O photochemical regimes over LFS revealed NO-limited throughout the period. NO increased first, reaching peak in 2011, followed by substantial decrease; while HCHO exhibited significant increase, contributing to decreasing trend in MDA8 O during 2006-2015. The plateauing NO and decreasing HCHO may contribute to the increase in MDA8 O in 2016. Subsequently, both NO and HCHO exhibited notable fluctuations, leading to significant changes in O. The study results fill the gap in the understanding of long-term O trends in high-latitude areas in the Northeast China Plain and offer valuable insights for assessing the impact of O on crop yields, forest productivity, and climate change.
地面臭氧(O)是一种关键的空气污染物,它会影响空气质量、人类健康、农业生产和气候变化。研究地面臭氧的长期变化及其影响因素对于了解臭氧污染及其影响至关重要。本研究在东北平原东北部的龙凤山区域大气背景站(LFS;44.44°N,127.36°E,330.5 m a.s.l.)进行了 2006-2022 年期间的地面臭氧长期变化分析。最大日 8 小时滑动平均值(MDA8)的地面臭氧波动较大,2006-2015 年期间,MDA8 年递减率显著(-0.62 ppb yr,p < 0.05),2015-2016 年出现跃升,2020-2022 年明显增加。利用气象变量建立 MDA8 的逐步多元线性回归模型,分解臭氧变化的人为和气象贡献。人为活动是 MDA8 地面臭氧长期趋势的主要驱动因素,占 MDA8 臭氧年变化的 73%,而气象的作用相对较小(27%)。LFS 地面臭氧升高主要与来自华北平原、东北平原和华北沿海地区的气流有关,主要发生在暖季(5-10 月)。基于卫星产品的 NO 和 HCHO 柱,LFS 的 O 光化学反应区在整个时期都呈现出氮限制。NO 先增加,在 2011 年达到峰值,随后大幅下降;而 HCHO 则显著增加,导致 2006-2015 年 MDA8 地面臭氧呈下降趋势。NO 的平稳和 HCHO 的减少可能导致 2016 年 MDA8 地面臭氧的增加。随后,NO 和 HCHO 都呈现出显著的波动,导致 O 的显著变化。研究结果填补了对东北平原高纬度地区长期地面臭氧趋势理解的空白,为评估地面臭氧对作物产量、森林生产力和气候变化的影响提供了有价值的见解。