Hydraulic transmissivity inferred from ice-sheet relaxation following Greenland supraglacial lake drainages
Hydraulic transmissivity under the 1km-thick Greenland Ice Sheet was inferred by ice-sheet uplift relaxation after rapid lake drainage events. A two-order-of-magnitude increase in hydraulic transmissivity was found throughout the melt season.
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Auteurs principaux: | , , , , , , |
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Format: | article |
Langue: | EN |
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Nature Portfolio
2021
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Accès en ligne: | https://doaj.org/article/bb6ae85caece42c5a2d0edbfbec7eb19 |
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