Long-term support of an active subglacial hydrologic system in Southeast Greenland by firn aquifers
Plain language summary: The flow of ice and meltwater from the Greenland Ice Sheet into the ocean affects sea levels. Ice flow is sensitive to meltwater that travels underneath the glacier. Where and when that water reaches the glacier bed shapes the water channel network under the glacier. We use a...
| Published in: | Geophysical Research Letters |
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| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
American Geophysical Union
2019
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| Subjects: | |
| Online Access: | http://hdl.handle.net/10477/79482 https://doi.org/10.1029/2019GL082786 |
| Summary: | Plain language summary: The flow of ice and meltwater from the Greenland Ice Sheet into the ocean affects sea levels. Ice flow is sensitive to meltwater that travels underneath the glacier. Where and when that water reaches the glacier bed shapes the water channel network under the glacier. We use a computer model to analyze how firn aquifers, newly discovered meltwater pockets that sit dozens of meters below the ice-sheet surface in East Greenland, change the water channel network under local glaciers. We find that the firn-aquifer water supply can maintain a water channel network under the glacier that changes less over each season, compared to areas without firn-aquifer water. This subglacial channelization could explain observations of steadier glacier flow in locations with firn aquifers. The state of the subglacial hydrologic system, which can modify ice motion, is sensitive to the volume and rate of meltwater reaching it. Bare-ice regions rapidly transport meltwater to the bed via moulins, while in certain accumulation-zone regions, meltwater first flows through firn aquifers, which can introduce a substantial delay. We use a subglacial hydrological model forced with idealized meltwater input scenarios to test the effect of this delay on subglacial hydrology. We find that addition of firn-aquifer water to the subglacial system elevates the inland subglacial water pressure while reducing water pressure and enhancing subglacial channelization near the terminus. This effect dampens seasonal variations in subglacial water pressure and may explain regionally anomalous ice-velocity patterns observed in Southeast Greenland. As surface melt rates increase and firn aquifers expand inland, it is crucial to understand how inland drainage of meltwater affects the evolution of the subglacial hydrologic system. K.P. was supported by an appointment to the NASA Postdoctoral Program at NASA Goddard Space Flight Center, administered by Universities Space Research Association, and by the Research and Education in eNergy, Environment and Water (RENEW) Institute. L.C.A. acknowledges support from the Global Modeling and Assimilation Office at NASA Goddard Space Flight Center funded under the NASA Modeling, Analysis, and Prediction (MAP) program. C.F.D. was supported by the Canada Research Chairs Programme and the Natural Sciences and Engineering Research Council of Canada. The model simulations were performed using resources provided by Compute Canada. |
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