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

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

<p>Mid-latitude mountain glaciers are sensitive to local summer temperature changes. Chronologies of past glacier fluctuations based on the investigation of glacial landforms therefore allow for a better understanding of natural climate variability at local scale, which is relevant for the ass...

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Bibliographic Details
Main Authors: I. Schimmelpfennig, J. M. Schaefer, J. Lamp, V. Godard, R. Schwartz, E. Bard, T. Tuna, N. Akçar, C. Schlüchter, S. Zimmerman
Format: Article
Language:English
Published: Copernicus Publications 2022-01-01
Series:Climate of the Past
Online Access:https://cp.copernicus.org/articles/18/23/2022/cp-18-23-2022.pdf

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https://cp.copernicus.org/articles/18/23/2022/cp-18-23-2022.pdf

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