Modeling Maximum and Minimum Neogene Antarctic Ice Sheets
{'Code': '01020301', 'Directorate': {'Abbreviation': 'O/D', 'LongName': 'Office Of The Director'}, 'Division': {'Abbreviation': 'OPP', 'LongName': 'Office of Polar Programs'}}
{'SignBlockName': 'Mary Campbell', 'PO_EMAI': None, 'PO_PHON': None}
About 2.4 million years ago, our relatively warm plant with an ice              budget confined to Antarctica was thrust into late Cenzoic global               ice ages with pulsating ice sheets at both poles.  A fundamental                scientific question is the nature of warm-earth climate dynamics                in the few million years preceding this change.  The objective of               this project is to test the primary hypotheses for maximum and                  minimum ice sheet configuration during the late Neogene using a                 finite-element model of the Antarctic Ice Sheet.  The synergism                 that will be applied between Antarctic continent glacial geology,               the deep-sea 18-0 record, and ice physics provides constraints                  sufficient to limit significantly possible ice sheet variations.                The numerical ice sheet reconstructions that result will best                   satisfy  available data and have an impact on our understanding of              global environmental change.
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[{'Code': '5112', 'Text': 'ANT Earth Sciences'}, {'Code': '5116', 'Text': 'ANT Glaciology'}]
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