Articles | Volume 18, issue 1
https://doi.org/10.5194/cp-18-23-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-18-23-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
14 Jan 2022
Research article |
| 14 Jan 2022
| 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
CORRESPONDING AUTHOR
Aix-Marseille Université, CNRS, Coll France, IRD, INRAE, CEREGE, Aix en Provence, France
Joerg M. Schaefer
Lamont-Doherty Earth Observatory of Columbia University, Geochemistry, Palisades, NY 10964, USA
Jennifer Lamp
Lamont-Doherty Earth Observatory of Columbia University, Geochemistry, Palisades, NY 10964, USA
Vincent Godard
Aix-Marseille Université, CNRS, Coll France, IRD, INRAE, CEREGE, Aix en Provence, France
Roseanne Schwartz
Lamont-Doherty Earth Observatory of Columbia University, Geochemistry, Palisades, NY 10964, USA
Edouard Bard
Aix-Marseille Université, CNRS, Coll France, IRD, INRAE, CEREGE, Aix en Provence, France
Thibaut Tuna
Aix-Marseille Université, CNRS, Coll France, IRD, INRAE, CEREGE, Aix en Provence, France
Naki Akçar
Institute of Geological Sciences, University of Bern, Bern,
Switzerland
Christian Schlüchter
Institute of Geological Sciences, University of Bern, Bern,
Switzerland
Susan Zimmerman
Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, CA 94550, USA
A full list of authors appears at the end of the paper.
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Revised manuscript not accepted
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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.
Small mountain glaciers advance and recede as a response to summer temperature changes. Dating...
