Articles | Volume 22, issue 16
https://doi.org/10.5194/acp-22-10425-2022
https://doi.org/10.5194/acp-22-10425-2022
Research article
 | 
16 Aug 2022
Research article |  | 16 Aug 2022

Ozone–gravity wave interaction in the upper stratosphere/lower mesosphere

Axel Gabriel

Viewed

Total article views: 1,681 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,153 468 60 1,681 31 29
  • HTML: 1,153
  • PDF: 468
  • XML: 60
  • Total: 1,681
  • BibTeX: 31
  • EndNote: 29
Views and downloads (calculated since 03 Jan 2022)
Cumulative views and downloads (calculated since 03 Jan 2022)

Viewed (geographical distribution)

Total article views: 1,681 (including HTML, PDF, and XML) Thereof 1,803 with geography defined and -122 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Nov 2024
Download
Short summary
Recent measurements show some evidence that the amplitudes of atmospheric gravity waves (horizontal wavelengths of 100–2000 km), which propagate from the troposphere (0–10 km) to the stratosphere and mesosphere (10–100 km), increase more strongly with height during daytime than during nighttime. This study shows that ozone–temperature coupling in the upper stratosphere can principally produce such an amplification. The results will help to improve atmospheric circulation models.
Altmetrics
Final-revised paper
Preprint