Articles | Volume 39, issue 1
https://doi.org/10.5194/angeo-39-267-2021
https://doi.org/10.5194/angeo-39-267-2021
Regular paper
 | 
01 Mar 2021
Regular paper |  | 01 Mar 2021

Stratospheric influence on the mesosphere–lower thermosphere over mid latitudes in winter observed by a Fabry–Perot interferometer

Olga S. Zorkaltseva and Roman V. Vasilyev

Viewed

Total article views: 1,736 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,286 402 48 1,736 32 29
  • HTML: 1,286
  • PDF: 402
  • XML: 48
  • Total: 1,736
  • BibTeX: 32
  • EndNote: 29
Views and downloads (calculated since 10 Nov 2020)
Cumulative views and downloads (calculated since 10 Nov 2020)

Viewed (geographical distribution)

Total article views: 1,736 (including HTML, PDF, and XML) Thereof 1,544 with geography defined and 192 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 26 Apr 2024
Download
Short summary
One of the fundamental tasks of atmospheric physics is the study of the processes of vertical interaction of atmospheric layers. We carried out observations with a Fabry–Perot interferometer at an altitude of 90–100 km. We have shown that sudden stratospheric warming and active planetary waves have an impact on the dynamics of the upper atmosphere. That is, the green line airglow decreases and the temperature rises. Major warming causes the reversal of the zonal wind in the upper atmosphere.