In situ cosmogenic <sup>10</sup>Be–<sup>14</sup>C–<sup>26</sup>Al measurements from recently deglaciated bedrock as a new tool to decipher changes in Greenland Ice Sheet size

In situ cosmogenic <sup>10</sup>Be–<sup>14</sup>C–<sup>26</sup>Al measurements from recently deglaciated bedrock as a new tool to decipher changes in Greenland Ice Sheet size

<p>Sometime during the middle to late Holocene (8.2 <span class="inline-formula">ka</span> to <span class="inline-formula">∼</span> 1850–1900 CE), the Greenland Ice Sheet (GrIS) was smaller than its current configuration. Determining the exact dimens...

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Bibliographic Details
Main Authors: N. E. Young, A. J. Lesnek, J. K. Cuzzone, J. P. Briner, J. A. Badgeley, A. Balter-Kennedy, B. L. Graham, A. Cluett, J. L. Lamp, R. Schwartz, T. Tuna, E. Bard, M. W. Caffee, S. R. H. Zimmerman, J. M. Schaefer
Format: Article
Language:English
Published: Copernicus Publications 2021-02-01
Series:Climate of the Past
Online Access:https://cp.copernicus.org/articles/17/419/2021/cp-17-419-2021.pdf

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https://cp.copernicus.org/articles/17/419/2021/cp-17-419-2021.pdf

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