Articles | Volume 25, issue 14
https://doi.org/10.5194/acp-25-8029-2025
https://doi.org/10.5194/acp-25-8029-2025
Research article
 | 
28 Jul 2025
Research article |  | 28 Jul 2025

Distinct structures of interannual variations in stratosphere-to-troposphere ozone transport induced by the Tibetan Plateau thermal forcing

Qingjian Yang, Tianliang Zhao, Yongqing Bai, Kai Meng, Yuehan Luo, Zhijie Tian, Xiaoyun Sun, Weikang Fu, Kai Yang, and Jun Hu

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Cited articles

Akritidis, D., Pozzer, A., Zanis, P., Tyrlis, E., Škerlak, B., Sprenger, M., and Lelieveld, J.: On the role of tropopause folds in summertime tropospheric ozone over the eastern Mediterranean and the Middle East, Atmos. Chem. Phys., 16, 14025–14039, https://doi.org/10.5194/acp-16-14025-2016, 2016. 
Ancellet, G., Beekmann, M., and Papayannis, A.: Impact of a cutoff low development on downward transport of ozone in the troposphere, J. Geophys. Res.-Atmos., 99, 3451–3468, https://doi.org/10.1029/93JD02551, 1994. 
Chen, W., Liao, H., and Seinfeld, J. H.: Future climate impacts of direct radiative forcing of anthropogenic aerosols, tropospheric ozone, and long-lived greenhouse gases, J. Geophys. Res., 112, 2006JD008051, https://doi.org/10.1029/2006JD008051, 2007. 
Cressman, G. P.: Circulations of the West Pacific jet stream, Mon. Weather Rev., 109, 2450–2463, https://doi.org/10.1175/1520-0493(1981)109<2450:COTWPJ>2.0.CO;2, 1981. 
Ding, A. and Wang, T.: Influence of stratosphere-to-troposphere exchange on the seasonal cycle of surface ozone at Mount Waliguan in western China, Geophys. Res. Lett., 33, L03803, https://doi.org/10.1029/2005GL024760, 2006. 
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This study reveals a unique driver of the Tibetan Plateau (TP) thermal forcing of the interannual variations in stratosphere-to-troposphere transport (STT) of ozone with diverse structures. Anomalous strong TP thermal forcing induces anticyclonic anomalies in the upper troposphere over the TP, which strengthens and attenuates the northern and southern branches of the westerly jet, intensifying (weakening) the westerly trough for more (fewer) tropopause folds of ozone STT over the East Asian region.
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