Greenland supraglacial lake drainages triggered by hydrologically induced basal slip
Water-driven fracture propagation beneath supraglacial lakes rapidly transports large volumes of surface meltwater to the base of the Greenland Ice Sheet1. These drainage events drive transient ice-sheet acceleration1,2,3 and establish conduits for additional surface-to-bed meltwater transport for t...
| Päätekijät: | , , , , , , , |
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| Aineistotyyppi: | Journal article |
| Kieli: | English |
| Julkaistu: |
Springer Nature
2015
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