Articles | Volume 18, issue 1
https://doi.org/10.5194/cp-18-23-2022
https://doi.org/10.5194/cp-18-23-2022
Research article
 | 
14 Jan 2022
Research article |  | 14 Jan 2022

Glacier response to Holocene warmth inferred from in situ 10Be and 14C bedrock analyses in Steingletscher's forefield (central Swiss Alps)

Irene Schimmelpfennig, Joerg M. Schaefer, Jennifer Lamp, Vincent Godard, Roseanne Schwartz, Edouard Bard, Thibaut Tuna, Naki Akçar, Christian Schlüchter, Susan Zimmerman, and ASTER Team

Viewed

Total article views: 3,972 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,945 946 81 3,972 49 56
  • HTML: 2,945
  • PDF: 946
  • XML: 81
  • Total: 3,972
  • BibTeX: 49
  • EndNote: 56
Views and downloads (calculated since 02 Sep 2021)
Cumulative views and downloads (calculated since 02 Sep 2021)

Viewed (geographical distribution)

Total article views: 3,972 (including HTML, PDF, and XML) Thereof 3,710 with geography defined and 262 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 29 Jun 2024
Download
Short summary
Small mountain glaciers advance and recede as a response to summer temperature changes. Dating of glacial landforms with cosmogenic nuclides allowed us to reconstruct the advance and retreat history of an Alpine glacier throughout the past ~ 11 000 years, the Holocene. The results contribute knowledge to the debate of Holocene climate evolution, indicating that during most of this warm period, summer temperatures were similar to or warmer than in modern times.