Cryosphere: 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.

Bibliographic Details
Main Author: Jeffrey Evans
Format: Other Non-Article Part of Journal/Newspaper
Language:unknown
Published: 2015
Subjects:
Earth Sciences not elsewhere classified
untagged
Antarctic
Antarc*
Ice Sheet
Online Access:https://figshare.com/articles/journal_contribution/Cryosphere_Antarctic_ice_growth_and_retreat/9481487
id ftloughboroughun:oai:figshare.com:article/9481487
record_format openpolar
spelling ftloughboroughun:oai:figshare.com:article/9481487 2023-05-15T13:35:35+02:00 Cryosphere: Antarctic ice growth and retreat Jeffrey Evans 2015-01-01T00:00:00Z https://figshare.com/articles/journal_contribution/Cryosphere_Antarctic_ice_growth_and_retreat/9481487 unknown 2134/18720 https://figshare.com/articles/journal_contribution/Cryosphere_Antarctic_ice_growth_and_retreat/9481487 CC BY-NC-ND 4.0 CC-BY-NC-ND Earth Sciences not elsewhere classified untagged Text Journal contribution 2015 ftloughboroughun 2022-01-01T20:19:10Z 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. Other Non-Article Part of Journal/Newspaper Antarc* Antarctic Ice Sheet Loughborough University: Figshare Antarctic
institution Open Polar
collection Loughborough University: Figshare
op_collection_id ftloughboroughun
language unknown
topic Earth Sciences not elsewhere classified
untagged
spellingShingle Earth Sciences not elsewhere classified
untagged
Jeffrey Evans
Cryosphere: Antarctic ice growth and retreat
topic_facet Earth Sciences not elsewhere classified
untagged
description 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.
format Other Non-Article Part of Journal/Newspaper
author Jeffrey Evans
author_facet Jeffrey Evans
author_sort Jeffrey Evans
title Cryosphere: Antarctic ice growth and retreat
title_short Cryosphere: Antarctic ice growth and retreat
title_full Cryosphere: Antarctic ice growth and retreat
title_fullStr Cryosphere: Antarctic ice growth and retreat
title_full_unstemmed Cryosphere: Antarctic ice growth and retreat
title_sort cryosphere: antarctic ice growth and retreat
publishDate 2015
url https://figshare.com/articles/journal_contribution/Cryosphere_Antarctic_ice_growth_and_retreat/9481487
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Ice Sheet
genre_facet Antarc*
Antarctic
Ice Sheet
op_relation 2134/18720
https://figshare.com/articles/journal_contribution/Cryosphere_Antarctic_ice_growth_and_retreat/9481487
op_rights CC BY-NC-ND 4.0
op_rightsnorm CC-BY-NC-ND
_version_ 1766067466303176704

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