High geothermal heat flow beneath Thwaites Glacier in West Antarctica inferred from aeromagnetic data
Geothermal heat flow in the polar regions plays a crucial role in understanding ice-sheet dynamics and predictions of sea level rise. Continental-scale indirect estimates often have a low spatial resolution and yield largest discrepancies in West Antarctica. Here we analyse geophysical data to estim...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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Springer Nature
2021
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Online Access: | https://epic.awi.de/id/eprint/54536/ https://epic.awi.de/id/eprint/54536/1/Dziadek-etal_high-geothermal-heatflow-ASE-ThaitesGlacier_CommsEarthEnviron_2021.pdf https://epic.awi.de/id/eprint/54536/2/Dziadek-etal_high-geothermal-heatflow-ASE-ThaitesGlacier_CommsEarthEnviron_2021_SuppInfo.pdf https://hdl.handle.net/10013/epic.fe5cb742-fc28-49a1-a3d7-2a7b080d72b9 https://hdl.handle.net/ |