Articles | Volume 39, issue 2
https://doi.org/10.5194/angeo-39-357-2021
https://doi.org/10.5194/angeo-39-357-2021
Regular paper
 | 
14 Apr 2021
Regular paper |  | 14 Apr 2021

Modelling the residual mean meridional circulation at different stages of sudden stratospheric warming events

Andrey V. Koval, Wen Chen, Ksenia A. Didenko, Tatiana S. Ermakova, Nikolai M. Gavrilov, Alexander I. Pogoreltsev, Olga N. Toptunova, Ke Wei, Anna N. Yarusova, and Anton S. Zarubin

Viewed

Total article views: 1,924 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,401 464 59 1,924 54 54
  • HTML: 1,401
  • PDF: 464
  • XML: 59
  • Total: 1,924
  • BibTeX: 54
  • EndNote: 54
Views and downloads (calculated since 23 Oct 2020)
Cumulative views and downloads (calculated since 23 Oct 2020)

Viewed (geographical distribution)

Total article views: 1,924 (including HTML, PDF, and XML) Thereof 1,814 with geography defined and 110 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 26 Dec 2024
Download
Short summary
Numerical modelling is used to simulate atmospheric circulation and calculate residual mean meridional circulation (RMC) during sudden stratospheric warming (SSW) events. Calculating the RMC is used to take into account wave effects on the transport of atmospheric quantities and gas species in the meridional plane. The results show that RMC undergoes significant changes at different stages of SSW and contributes to SSW development.