Articles | Volume 16, issue 12
https://doi.org/10.5194/tc-16-4887-2022
https://doi.org/10.5194/tc-16-4887-2022
Research article
 | 
06 Dec 2022
Research article |  | 06 Dec 2022

New 10Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica

Jonathan R. Adams, Joanne S. Johnson, Stephen J. Roberts, Philippa J. Mason, Keir A. Nichols, Ryan A. Venturelli, Klaus Wilcken, Greg Balco, Brent Goehring, Brenda Hall, John Woodward, and Dylan H. Rood

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Cited articles

Ackert, R. P., Barclay, D. J., Borns, H. W., Calkin, P. E., Kurz, M. D., Fastook, J. L., and Steig, E. J.: Measurements of past ice sheet elevations in interior West Antarctica, Science, 286, 276–280, https://doi.org/10.1126/science.286.5438.276, 1999. 
Adams, J. R., Rood, D. H., Wilcken, K., Roberts, S. J., and Johnson J. S.: Beryllium-10 exposure ages for Pope Glacier from a scoria cone 1.5 km west of Mount Murphy in the Amundsen Sea Embayment (Version 1.0), NERC EDS UK Polar Data Centre [data set], https://doi.org/10.5285/8F275626-5F22-48DF-95E5-CDC8F204A897, 2022. 
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Short summary
Glaciers in West Antarctica are experiencing significant ice loss. Geological data provide historical context for ongoing ice loss in West Antarctica, including constraints on likely future ice sheet behaviour in response to climatic warming. We present evidence from rare isotopes measured in rocks collected from an outcrop next to Pope Glacier. These data suggest that Pope Glacier thinned faster and sooner after the last ice age than previously thought.
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