Pine Island Glacier on West Antarctica's Amundsen Sea coast has experienced accelerating retreat over the past few decades. Oceanographic observations under the associated ice shelf show how changes in water flow and ice-cavity geometry have contributed to ice melting.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 12 print issues and online access
$259.00 per year
only $21.58 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Jenkins, A. et al. Nature Geosci. 10.1038/ngeo890 (2010).
Wingham, D. J., Shepherd, A., Muir, A. & Marshall, G. J. Phil. Trans. R. Soc. A 364, 1627–1635 (2006).
Rignot, E. et al. Nature Geosci. 1, 106–110 (2008).
Jacobs, S. S., Hellmer, H. H. & Jenkins, A. Geophys. Res. Lett. 23, 957–960 (1996).
Shepherd, A., Wingham, D. & Rignot, E. Geophys. Res. Lett. 31, L23402 (2004).
Schoof, C. J. Geophys. Res. 112, F03S28 (2007).
Goldberg, D., Holland, D. M. & Schoof, C. J. Geophys. Res. 114, F04026 (2009).
Dupont, T. K. & Alley, R. B. Geophys. Res. Lett. 32, L04503 (2005).
Holland, P., Jenkins, A. & Holland, D. M. J. Climate 21, 2558–2572 (2007).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Schoof, C. Beneath a floating ice shelf. Nature Geosci 3, 450–451 (2010). https://doi.org/10.1038/ngeo895
Published:
Issue Date:
DOI: https://doi.org/10.1038/ngeo895