4.7 Article

Influences of stratospheric intrusions to high summer surface ozone over a heavily industrialized region in northern China

Journal

ENVIRONMENTAL RESEARCH LETTERS
Volume 17, Issue 9, Pages -

Publisher

IOP Publishing Ltd
DOI: 10.1088/1748-9326/ac8b24

Keywords

stratospheric intrusion; GNAQPMS; surface ozone; NCP

Funding

  1. Cultivating Project of Strategic Priority Research Program of Chinese Academy of Sciences [XDPB1903]
  2. Strategic Priority Research Program of the Chinese Academy of Sciences [XDA19040202]
  3. National Natural Science Foundation of China [92044302, 91744203]

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This study investigates the impact of a stratospheric-to-tropospheric transport event on surface high ozone episodes over heavily industrialized regions in northern China during summer. The results show that the stratospheric contribution has a certain influence on surface high ozone events in the target region, which is important for understanding the influence of natural processes in heavily polluted areas during summer.
The stratospheric contribution to tropospheric ozone has long been a topic of much debate over the past few decades. In this study, we leveraged multiple datasets from surface, sounding and satellite observations to reanalysis datasets, along with a global chemical transport model (Global Nested Air Quality Prediction Modelling System, GNAQPMS) to investigate the impact of a stratospheric-to-tropospheric transport (STT) event characterized by long duration and wide range in the summer on surface high ozone episodes over heavily industrialized regions in northern China. In 14-18 August 2019, the ERA5 reanalysis datasets showed a potential vorticity (PV) tongue and a deep, upper-level trough penetrate towards 35 degrees N over the North China Plain (NCP), indicating the occurrence of a stratospheric intrusion. From Atmospheric Infrared Sounder (AIRS) measurements, we found that the ozone-rich, stratospheric air mass had been injected into the lower altitudes. The GNAQPMS generally captured the featured layers, although there was a slight underestimation in the low troposphere. The averaged magnitudes of stratospheric contribution (O3S) and percentage (O3F) simulated by GNAQPMS were 3-20 mu g m(-3) and 6%-20%, respectively, while the Whole Atmosphere Community Climate Model (WACCM) indicated a higher stratospheric contribution by 3-5 mu g m(-3). Through this study, we give our opinions on the controversial topic of a more thorough understanding of the influence of natural processes apart from anthropogenic emissions, even in a heavily polluted region during summer.

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