Articles | Volume 13, issue 2
https://doi.org/10.5194/tc-13-627-2019
https://doi.org/10.5194/tc-13-627-2019
Research article
 | 
20 Feb 2019
Research article |  | 20 Feb 2019

Leads and ridges in Arctic sea ice from RGPS data and a new tracking algorithm

Nils Hutter, Lorenzo Zampieri, and Martin Losch

Viewed

Total article views: 3,859 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,673 1,112 74 3,859 90 69
  • HTML: 2,673
  • PDF: 1,112
  • XML: 74
  • Total: 3,859
  • BibTeX: 90
  • EndNote: 69
Views and downloads (calculated since 02 Oct 2018)
Cumulative views and downloads (calculated since 02 Oct 2018)

Viewed (geographical distribution)

Total article views: 3,859 (including HTML, PDF, and XML) Thereof 3,414 with geography defined and 445 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 18 Apr 2024
Download
Short summary
Arctic sea ice is an aggregate of ice floes with various sizes. The different sizes result from constant deformation of the ice pack. If a floe breaks, open ocean is exposed in a lead. Collision of floes forms pressure ridges. Here, we present algorithms that detect and track these deformation features in satellite observations and model output. The tracked features are used to provide a comprehensive description of localized deformation of sea ice and help to understand its material properties.