Articles | Volume 24, issue 6
https://doi.org/10.5194/acp-24-3759-2024
https://doi.org/10.5194/acp-24-3759-2024
Peer-reviewed comment
 | 
26 Mar 2024
Peer-reviewed comment |  | 26 Mar 2024

Comment on “Transport of substantial stratospheric ozone to the surface by a dying typhoon and shallow convection” by Chen et al. (2022)

Xiangdong Zheng, Wen Yang, Yuting Sun, Chunmei Geng, Yingying Liu, and Xiaobin Xu

Viewed

Total article views: 1,171 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
895 225 51 1,171 80 37 47
  • HTML: 895
  • PDF: 225
  • XML: 51
  • Total: 1,171
  • Supplement: 80
  • BibTeX: 37
  • EndNote: 47
Views and downloads (calculated since 01 Nov 2023)
Cumulative views and downloads (calculated since 01 Nov 2023)

Viewed (geographical distribution)

Total article views: 1,171 (including HTML, PDF, and XML) Thereof 1,154 with geography defined and 17 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 13 Dec 2024
Short summary
Chen et al. (2022) attributed the nocturnal ozone enhancement (NOE) during the night of 31 July 2021 in the North China Plain (NCP) to "the direct stratospheric intrusion to reach the surface". We analyzed in situ data from the NCP. Our results do not suggest that there was a significant impact from the stratosphere on surface ozone during the NOE. We argue that the NOE was not caused by stratospheric intrusion but originated from fresh photochemical production in the lower troposphere. 
Altmetrics
Final-revised paper
Preprint