Articles | Volume 1, issue 1
https://doi.org/10.5194/wcd-1-261-2020
https://doi.org/10.5194/wcd-1-261-2020
Research article
 | 
12 May 2020
Research article |  | 12 May 2020

Intermittency of Arctic–mid-latitude teleconnections: stratospheric pathway between autumn sea ice and the winter North Atlantic Oscillation

Peter Yu Feng Siew, Camille Li, Stefan Pieter Sobolowski, and Martin Peter King

Viewed

Total article views: 7,469 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
5,824 1,465 180 7,469 569 198 243
  • HTML: 5,824
  • PDF: 1,465
  • XML: 180
  • Total: 7,469
  • Supplement: 569
  • BibTeX: 198
  • EndNote: 243
Views and downloads (calculated since 14 Nov 2019)
Cumulative views and downloads (calculated since 14 Nov 2019)

Viewed (geographical distribution)

Total article views: 7,469 (including HTML, PDF, and XML) Thereof 6,587 with geography defined and 882 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 11 Jun 2026
Download
Short summary
Arctic sea ice loss has been linked to changes in mid-latitude weather and climate. However, the literature offers differing views on the strength, robustness, and even existence of these linkages. We use a statistical tool (Causal Effect Networks) to show that one proposed pathway linking Barents–Kara ice and mid-latitude circulation is intermittent in observations and likely only active under certain conditions. This result may help explain apparent inconsistencies across previous studies.
Share