Articles | Volume 10, issue 1
https://doi.org/10.5194/tc-10-245-2016
https://doi.org/10.5194/tc-10-245-2016
Research article
 | 
26 Jan 2016
Research article |  | 26 Jan 2016

Halogen-based reconstruction of Russian Arctic sea ice area from the Akademii Nauk ice core (Severnaya Zemlya)

A. Spolaor, T. Opel, J. R. McConnell, O. J. Maselli, G. Spreen, C. Varin, T. Kirchgeorg, D. Fritzsche, A. Saiz-Lopez, and P. Vallelonga

Viewed

Total article views: 4,415 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,514 1,556 345 4,415 378 209 215
  • HTML: 2,514
  • PDF: 1,556
  • XML: 345
  • Total: 4,415
  • Supplement: 378
  • BibTeX: 209
  • EndNote: 215
Views and downloads (calculated since 24 Aug 2015)
Cumulative views and downloads (calculated since 24 Aug 2015)

Cited

Saved (preprint)

Latest update: 18 Apr 2024
Download
Short summary
The role of sea ice in the Earth climate system is still under debate, although it is known to influence albedo, ocean circulation, and atmosphere-ocean heat and gas exchange. Here we present a reconstruction of 1950 to 1998 AD sea ice in the Laptev Sea based on the Akademii Nauk ice core (Severnaya Zemlya, Russian Arctic) and halogen measurements. The results suggest a connection between bromine and sea ice, as well as a connection between iodine concentration in snow and summer sea ice.