Statistical appraisal of geothermal heat flow observations in the Arctic
<p>Geothermal heat flow is an important boundary condition for ice sheets, affecting, for example, basal melt rates, but for ice-covered regions, we only have sparse heat flow observations with partly high uncertainty of up to 30 m W m<span class="inline-formula"><sup>−2&...
| Main Authors: | , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2024-04-01
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| Series: | Solid Earth |
| Online Access: | https://se.copernicus.org/articles/15/513/2024/se-15-513-2024.pdf |