2012 refrozen melt layer location, density, and connectivity records from airborne radar sounding, Greenland, 2017
Surface meltwater runoff dominates present-day mass loss from the Greenland Ice Sheet. In the interior, porous firn can buffer runoff by retaining meltwater unless perched impermeable horizons, such as ice slabs, develop and restrict percolation. Recent field observations suggest that such horizons...
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| Format: | Dataset |
| Language: | unknown |
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Arctic Data Center
2021
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| Online Access: | https://doi.org/10.18739/A2736M33W |