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: 5,591 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
4,281 1,185 125 5,591 419 117 121
  • HTML: 4,281
  • PDF: 1,185
  • XML: 125
  • Total: 5,591
  • Supplement: 419
  • BibTeX: 117
  • EndNote: 121
Views and downloads (calculated since 14 Nov 2019)
Cumulative views and downloads (calculated since 14 Nov 2019)

Viewed (geographical distribution)

Total article views: 5,591 (including HTML, PDF, and XML) Thereof 4,799 with geography defined and 792 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 May 2025
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