Articles | Volume 14, issue 11
https://doi.org/10.5194/tc-14-4201-2020
https://doi.org/10.5194/tc-14-4201-2020
Research article
 | 
25 Nov 2020
Research article |  | 25 Nov 2020

Analyzing links between simulated Laptev Sea sea ice and atmospheric conditions over adjoining landmasses using causal-effect networks

Zoé Rehder, Anne Laura Niederdrenk, Lars Kaleschke, and Lars Kutzbach

Viewed

Total article views: 2,630 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,657 899 74 2,630 78 87
  • HTML: 1,657
  • PDF: 899
  • XML: 74
  • Total: 2,630
  • BibTeX: 78
  • EndNote: 87
Views and downloads (calculated since 10 Mar 2020)
Cumulative views and downloads (calculated since 10 Mar 2020)

Viewed (geographical distribution)

Total article views: 2,630 (including HTML, PDF, and XML) Thereof 2,502 with geography defined and 128 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 12 Jun 2024
Download
Short summary
To better understand the connection between sea ice and permafrost, we investigate how sea ice interacts with the atmosphere over the adjacent landmass in the Laptev Sea region using a climate model. Melt of sea ice in spring is mainly controlled by the atmosphere; in fall, feedback mechanisms are important. Throughout summer, lower-than-usual sea ice leads to more southward transport of heat and moisture, but these links from sea ice to the atmosphere over land are weak.