Journal cover Journal topic
Climate of the Past An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

IF value: 3.536
IF3.536
IF 5-year value: 3.967
IF 5-year
3.967
CiteScore value: 6.6
CiteScore
6.6
SNIP value: 1.262
SNIP1.262
IPP value: 3.90
IPP3.90
SJR value: 2.185
SJR2.185
Scimago H <br class='widget-line-break'>index value: 71
Scimago H
index
71
h5-index value: 40
h5-index40
Download
Short summary
The Colle Gnifetti (CG) glacier is the only drilling site in the European Alps offering ice core records back to some 1000 years. We aim to fully exploit these unique long-term records by establishing a reliable long-term age scale and an improved ice core proxy interpretation for reconstructing temperature. Our findings reveal a site-specific temperature-related signal in the trends of the mineral dust proxy Ca2+ that may supplement other proxy evidence over the last millennium.
CP | Articles | Volume 14, issue 1
Clim. Past, 14, 21–37, 2018
https://doi.org/10.5194/cp-14-21-2018
Clim. Past, 14, 21–37, 2018
https://doi.org/10.5194/cp-14-21-2018

Research article 10 Jan 2018

Research article | 10 Jan 2018

Temperature and mineral dust variability recorded in two low-accumulation Alpine ice cores over the last millennium

Pascal Bohleber et al.

Viewed

Total article views: 3,361 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,228 1,017 116 3,361 339 63 84
  • HTML: 2,228
  • PDF: 1,017
  • XML: 116
  • Total: 3,361
  • Supplement: 339
  • BibTeX: 63
  • EndNote: 84
Views and downloads (calculated since 16 Jun 2017)
Cumulative views and downloads (calculated since 16 Jun 2017)

Viewed (geographical distribution)

Total article views: 3,212 (including HTML, PDF, and XML) Thereof 3,194 with geography defined and 18 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 16 Jan 2021
Publications Copernicus
Download
Short summary
The Colle Gnifetti (CG) glacier is the only drilling site in the European Alps offering ice core records back to some 1000 years. We aim to fully exploit these unique long-term records by establishing a reliable long-term age scale and an improved ice core proxy interpretation for reconstructing temperature. Our findings reveal a site-specific temperature-related signal in the trends of the mineral dust proxy Ca2+ that may supplement other proxy evidence over the last millennium.
Citation