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

Bohleber, Pascal; Erhardt, Tobias; Spaulding, Nicole; Hoffmann, Helene; Fischer, Hubertus; Mayewski, Paul

doi:https://doi.org/10.5194/cp-14-21-2018

Articles | Volume 14, issue 1

Clim. Past, 14, 21–37, 2018

https://doi.org/10.5194/cp-14-21-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Clim. Past, 14, 21–37, 2018

https://doi.org/10.5194/cp-14-21-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 14, issue 1

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.

Supplement

https://doi.org/10.5194/cp-14-21-2018-supplement

Data sets

Temperature and mineral dust variability recorded of ice core Colle_Gnifetti_KCC, PANGAEA P. Bohleber, T. Erhardt, N. Spaulding, H. Hoffmann, H. Fischer, and P. Mayewski: https://doi.org/10.1594/PANGAEA.883521

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.