Evans_Nature Geoscience_doi10.1038ngeo2494.pdf (276.13 kB)
Download fileCryosphere: Antarctic ice growth and retreat
Antarctic Ice Sheet change during the last glacial cycle is unclear. The timing of moraine development in the Ross basin suggests that the ice sheet reached maximum thickness under the warming temperatures of the last termination.
History
School
- Social Sciences
Department
- Geography and Environment
Published in
NATURE GEOSCIENCEVolume
8Issue
8Pages
585 - 586 (2)Citation
EVANS, J., 2015. Cryosphere: Antarctic ice growth and retreat. Nature Geoscience, 8 (8), pp.585-586Publisher
© Nature Publishing GroupVersion
- AM (Accepted Manuscript)
Publisher statement
This work is made available according to the conditions of the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0) licence. Full details of this licence are available at: https://creativecommons.org/licenses/by-nc-nd/4.0/Publication date
2015ISSN
1752-0894Publisher version
Language
- en
