A Model of the Greenland Ice Sheet Deglaciation
The goal of this thesis is to improve our understanding of the Greenland ice sheet (GrIS) and how it responds to climate change. This was achieved using ice core records to infer elevation changes of the GrIS during the Holocene (11.7 ka BP to Present). The inferred elevation changes show the respon...
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| Language: | en |
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Université d'Ottawa / University of Ottawa
2013
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| Online Access: | http://hdl.handle.net/10393/30362 http://dx.doi.org/10.20381/ruor-3396 |