Articles | Volume 5, issue 1
https://doi.org/10.5194/wcd-5-231-2024
https://doi.org/10.5194/wcd-5-231-2024
Research article
 | 
19 Feb 2024
Research article |  | 19 Feb 2024

Stratospheric influence on the winter North Atlantic storm track in subseasonal reforecasts

Hilla Afargan-Gerstman, Dominik Büeler, C. Ole Wulff, Michael Sprenger, and Daniela I. V. Domeisen

Viewed

Total article views: 1,590 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,208 342 40 1,590 31 19
  • HTML: 1,208
  • PDF: 342
  • XML: 40
  • Total: 1,590
  • BibTeX: 31
  • EndNote: 19
Views and downloads (calculated since 18 Nov 2022)
Cumulative views and downloads (calculated since 18 Nov 2022)

Viewed (geographical distribution)

Total article views: 1,590 (including HTML, PDF, and XML) Thereof 1,555 with geography defined and 35 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 29 Jun 2024
Download
Short summary
The stratosphere is a layer of Earth's atmosphere found above the weather systems. Changes in the stratosphere can affect the winds and the storm tracks in the North Atlantic region for a relatively long time, lasting for several weeks and even months. We show that the stratosphere can be important for weather forecasts beyond 1 week, but more work is needed to improve the accuracy of these forecasts for 3–4 weeks.