Articles | Volume 17, issue 8
https://doi.org/10.5194/tc-17-3229-2023
https://doi.org/10.5194/tc-17-3229-2023
Research article
 | 
09 Aug 2023
Research article |  | 09 Aug 2023

Atmospheric highs drive asymmetric sea ice drift during lead opening from Point Barrow

MacKenzie E. Jewell, Jennifer K. Hutchings, and Cathleen A. Geiger

Viewed

Total article views: 1,269 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
863 341 65 1,269 90 61 56
  • HTML: 863
  • PDF: 341
  • XML: 65
  • Total: 1,269
  • Supplement: 90
  • BibTeX: 61
  • EndNote: 56
Views and downloads (calculated since 27 Jan 2023)
Cumulative views and downloads (calculated since 27 Jan 2023)

Viewed (geographical distribution)

Total article views: 1,269 (including HTML, PDF, and XML) Thereof 1,247 with geography defined and 22 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 10 Oct 2024
Download
Short summary
Sea ice repeatedly fractures near a prominent Alaskan headland as winds move ice along the coast, challenging predictions of sea ice drift. We find winds from high-pressure systems drive these fracturing events, and the Alaskan coastal boundary modifies the resultant ice drift. This observational study shows how wind patterns influence sea ice motion near coasts in winter. Identified relations between winds, ice drift, and fracturing provide effective test cases for dynamic sea ice models.