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High geothermal heat flux measured below the West Antarctic Ice Sheet
The geothermal heat flux is a critical thermal boundary condition that influences the melting, flow, and mass balance of ice sheets, but measurements of this parameter are difficult to make in ice-covered regions. We report the first direct measurement of geothermal heat flux into the base of the We...
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| Publicat a: | Sci Adv |
|---|---|
| Autors principals: | , , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
American Association for the Advancement of Science
2015
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4646773/ https://ncbi.nlm.nih.gov/pubmed/26601210 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.1500093 |
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