Evaluating different geothermal heat-flow maps as basal boundary conditions during spin-up of the Greenland ice sheet
<p>There is currently poor scientific agreement on whether the ice–bed interface is frozen or thawed beneath approximately one third of the Greenland ice sheet. This disagreement in basal thermal state results, at least partly, from differences in the subglacial geothermal heat-flow basal boun...
| Main Authors: | , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2024-01-01
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| Series: | The Cryosphere |
| Online Access: | https://tc.copernicus.org/articles/18/387/2024/tc-18-387-2024.pdf |