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A synthesis of the basal thermal state of the Greenland Ice Sheet
The basal thermal state of an ice sheet (frozen or thawed) is an important control upon its evolution, dynamics and response to external forcings. However, this state can only be observed directly within sparse boreholes or inferred conclusively from the presence of subglacial lakes. Here we synthes...
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| Pubblicato in: | J Geophys Res Earth Surf |
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| Autori principali: | , , , , , , , , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
2016
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5289704/ https://ncbi.nlm.nih.gov/pubmed/28163988 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1002/2015JF003803 |
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