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...

Full description

Bibliographic Details
Published in:The Cryosphere
Main Authors: N. Wilkens, J. Behrens, T. Kleiner, D. Rippin, M. Rückamp, A. Humbert
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2015
Subjects:
Online Access:https://doi.org/10.5194/tc-9-675-2015
https://doaj.org/article/f24252a8274a4494b50dc77784a29f22