Thermal structure and basal sliding parametrisation at Pine Island Glacier – a 3-D full-Stokes model study

Pine Island Glacier is one of the fastest changing glaciers of the Antarctic Ice Sheet and therefore of scientific interest. The glacier holds enough ice to raise the global sea level significantly (~ 0.5 m) when fully melted. The question addressed by numerous modelling studies of the glacier focus...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Wilkens, Nina, Behrens, Jörn, Kleiner, Thomas, Rippin, David M., Rückamp, Martin, Humbert, Angelika
Format: Article in Journal/Newspaper
Language:unknown
Published: COPERNICUS GESELLSCHAFT MBH 2015
Subjects:
Online Access:https://epic.awi.de/id/eprint/38895/
https://epic.awi.de/id/eprint/38895/1/tc-9-675-2015.pdf
https://doi.org/10.5194/tc-9-675-2015
https://hdl.handle.net/10013/epic.46149
https://hdl.handle.net/10013/epic.46149.d001