Articles | Volume 20, issue 23
https://doi.org/10.5194/acp-20-14669-2020
https://doi.org/10.5194/acp-20-14669-2020
Research article
 | 
02 Dec 2020
Research article |  | 02 Dec 2020

Role of equatorial waves and convective gravity waves in the 2015/16 quasi-biennial oscillation disruption

Min-Jee Kang, Hye-Yeong Chun, and Rolando R. Garcia

Viewed

Total article views: 1,867 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,177 651 39 1,867 238 53 40
  • HTML: 1,177
  • PDF: 651
  • XML: 39
  • Total: 1,867
  • Supplement: 238
  • BibTeX: 53
  • EndNote: 40
Views and downloads (calculated since 17 Aug 2020)
Cumulative views and downloads (calculated since 17 Aug 2020)

Viewed (geographical distribution)

Total article views: 1,867 (including HTML, PDF, and XML) Thereof 1,920 with geography defined and -53 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 21 Nov 2024
Short summary
In winter 2015/16, the descent of the westerly quasi-biennial oscillation (QBO) jet was interrupted by easterly winds. We find that Rossby–gravity and inertia–gravity waves weaken the jet core in early stages, and small-scale convective gravity waves, as well as horizontal and vertical components of Rossby waves, reverse the wind sign in later stages. The strong negative wave forcing in the tropics results from the enhanced convection, an anomalous wind profile, and barotropic instability.
Altmetrics
Final-revised paper
Preprint