Articles | Volume 33, issue 2
https://doi.org/10.5194/angeo-33-199-2015
https://doi.org/10.5194/angeo-33-199-2015
Regular paper
 | 
23 Feb 2015
Regular paper |  | 23 Feb 2015

The Hiccup: a dynamical coupling process during the autumn transition in the Northern Hemisphere – similarities and differences to sudden stratospheric warmings

V. Matthias, T. G. Shepherd, P. Hoffmann, and M. Rapp

Viewed

Total article views: 2,279 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,309 768 202 2,279 113 154
  • HTML: 1,309
  • PDF: 768
  • XML: 202
  • Total: 2,279
  • BibTeX: 113
  • EndNote: 154
Views and downloads (calculated since 23 Feb 2015)
Cumulative views and downloads (calculated since 23 Feb 2015)
Latest update: 19 Nov 2025
Download
Short summary
A vertical coupling process in the northern high-latitude middle atmosphere has been identified during the equinox transitions, which we call the “hiccup” and which acts like a “mini sudden stratospheric warming (SSW)”. We study the average characteristics of the hiccup based on a composite analysis using a nudged model. A comparison of the average characteristics of hiccups and SSWs shows both similarities and differences between the two vertical coupling processes.
Share