Articles | Volume 9, issue 6
https://doi.org/10.5194/tc-9-2253-2015
https://doi.org/10.5194/tc-9-2253-2015
Research article
 | 
04 Dec 2015
Research article |  | 04 Dec 2015

Investigation of a deep ice core from the Elbrus western plateau, the Caucasus, Russia

V. Mikhalenko, S. Sokratov, S. Kutuzov, P. Ginot, M. Legrand, S. Preunkert, I. Lavrentiev, A. Kozachek, A. Ekaykin, X. Faïn, S. Lim, U. Schotterer, V. Lipenkov, and P. Toropov

Viewed

Total article views: 3,678 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,689 1,805 184 3,678 131 154
  • HTML: 1,689
  • PDF: 1,805
  • XML: 184
  • Total: 3,678
  • BibTeX: 131
  • EndNote: 154
Views and downloads (calculated since 16 Jul 2015)
Cumulative views and downloads (calculated since 16 Jul 2015)

Cited

Saved (final revised paper)

Latest update: 17 Nov 2024
Download
Short summary
For the first time an ice core unaffected by melting was recovered from the western Elbrus plateau in the Caucasus. The preserved chemical and isotopic data are considered a source of paleo-climate information for southern/eastern Europe. Considerable snow accumulation (about 1500mm w.e.) and high sampling resolution allowed seasonal variability to be obtained in climate signals, covering a time period of about 200 years. Ice flow models suggest that the basal ice age can be more than 600 years.