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Ocean forcing of glacier retreat in the western Antarctic Peninsula

Cook, A.J.; Holland, P.R.; Meredith, M.P.; Murray, T.; Luckman, A.; Vaughan, D.G.

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Authors

A.J. Cook

P.R. Holland

M.P. Meredith

T. Murray

A. Luckman

D.G. Vaughan



Abstract

In recent decades, hundreds of glaciers draining the Antarctic Peninsula (63° to 70°S) have undergone systematic and progressive change. These changes are widely attributed to rapid increases in regional surface air temperature, but it is now clear that this cannot be the sole driver. Here, we identify a strong correspondence between mid-depth ocean temperatures and glacier-front changes along the ~1000-kilometer western coastline. In the south, glaciers that terminate in warm Circumpolar Deep Water have undergone considerable retreat, whereas those in the far northwest, which terminate in cooler waters, have not. Furthermore, a mid-ocean warming since the 1990s in the south is coincident with widespread acceleration of glacier retreat. We conclude that changes in ocean-induced melting are the primary cause of retreat for glaciers in this region.

Citation

Cook, A., Holland, P., Meredith, M., Murray, T., Luckman, A., & Vaughan, D. (2016). Ocean forcing of glacier retreat in the western Antarctic Peninsula. Science, 353(6296), 283-286. https://doi.org/10.1126/science.aae0017

Journal Article Type Article
Acceptance Date Jun 9, 2016
Online Publication Date Jul 15, 2016
Publication Date Jul 15, 2016
Deposit Date Jul 27, 2016
Publicly Available Date Aug 9, 2016
Journal Science
Print ISSN 0036-8075
Electronic ISSN 1095-9203
Publisher American Association for the Advancement of Science
Peer Reviewed Peer Reviewed
Volume 353
Issue 6296
Pages 283-286
DOI https://doi.org/10.1126/science.aae0017

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Accepted Journal Article (443 Kb)
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Copyright Statement
This is the author’s version of the work. It is posted here by permission of the AAAS for personal use, not for redistribution. The definitive version was published in Science on 15 Jul 2016: Vol. 353, Issue 6296, pp. 283-286, DOI: 10.1126/science.aae0017




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