Millennial-scale migration of the frozen/melted basal boundary, western Greenland ice sheet

The geometry and thermal structure of western Greenland ice sheet are known to have undergone relatively substantial change over the Holocene. Evolution of the frozen and melted fractions of the bed associated with the ice-sheet retreat over this time frame remains unclear. We address this question...

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Veröffentlicht in:	Journal of glaciology Jg. 68; H. 270; S. 775 - 784
Hauptverfasser:	Stansberry, Aidan, Harper, Joel, Johnson, Jesse V., Meierbachtol, Toby
Format:	Journal Article
Sprache:	Englisch
Veröffentlicht:	Cambridge, UK Cambridge University Press 01.08.2022
Schlagworte:	Basal ice Bedrock Fields Flowlines Geothermal power Glaciation Greenland ice sheet Heat conductivity Heat flux Heat sinks Heat transfer Heating Holocene Ice Ice ages Ice sheets ice temperature ice-sheet modeling Simulation Thermal structure Topography Greenland Basal ice ice temperature ice-sheet modeling
ISSN:	0022-1430, 1727-5652
Online-Zugang:	Volltext
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