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...
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Language: | English |
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American Geophysical Union
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Online Access: | http://hdl.handle.net/10477/79482 https://doi.org/10.1029/2019GL082786 |
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ftunivbuffalo:oai:ubir.buffalo.edu:10477/79482 2023-05-15T16:03:57+02:00 Long-term support of an active subglacial hydrologic system in Southeast Greenland by firn aquifers Poinar, Kristin Dow, Christine F. Andrews, Lauren C. 2019-04-29 http://hdl.handle.net/10477/79482 https://doi.org/10.1029/2019GL082786 en eng American Geophysical Union Datasets associated with article: http://hdl.handle.net/10477/79241 doi:10.1029/2019GL082786 Poinar, K., Dow, C.F., and Andrews, L.C. (2019). Long-term support of an active subglacial hydrologic system in Southeast Greenland by firn aquifers. Geophysical Research Letters, https://doi.org/10.1029/2019GL082786 http://hdl.handle.net/10477/79482 An edited version of this paper was published by AGU in Geophysical Research Letters. Copyright (2019) American Geophysical Union. Further reproduction or electronic distribution is not permitted. American Geophysical Union Greenland Ice Sheet ice sheet hydrology subglacial hydrology firn aquifer Article Video Preprint Text 2019 ftunivbuffalo https://doi.org/10.1029/2019GL082786 2022-02-20T06:33:07Z 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. Article in Journal/Newspaper East Greenland glacier glacier* Greenland Ice Sheet UBIR Repository (University at Buffalo Institutional Repository) Canada Greenland Geophysical Research Letters 46 9 4772 4781 |
institution |
Open Polar |
collection |
UBIR Repository (University at Buffalo Institutional Repository) |
op_collection_id |
ftunivbuffalo |
language |
English |
topic |
Greenland Ice Sheet ice sheet hydrology subglacial hydrology firn aquifer |
spellingShingle |
Greenland Ice Sheet ice sheet hydrology subglacial hydrology firn aquifer Poinar, Kristin Dow, Christine F. Andrews, Lauren C. Long-term support of an active subglacial hydrologic system in Southeast Greenland by firn aquifers |
topic_facet |
Greenland Ice Sheet ice sheet hydrology subglacial hydrology firn aquifer |
description |
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. |
format |
Article in Journal/Newspaper |
author |
Poinar, Kristin Dow, Christine F. Andrews, Lauren C. |
author_facet |
Poinar, Kristin Dow, Christine F. Andrews, Lauren C. |
author_sort |
Poinar, Kristin |
title |
Long-term support of an active subglacial hydrologic system in Southeast Greenland by firn aquifers |
title_short |
Long-term support of an active subglacial hydrologic system in Southeast Greenland by firn aquifers |
title_full |
Long-term support of an active subglacial hydrologic system in Southeast Greenland by firn aquifers |
title_fullStr |
Long-term support of an active subglacial hydrologic system in Southeast Greenland by firn aquifers |
title_full_unstemmed |
Long-term support of an active subglacial hydrologic system in Southeast Greenland by firn aquifers |
title_sort |
long-term support of an active subglacial hydrologic system in southeast greenland by firn aquifers |
publisher |
American Geophysical Union |
publishDate |
2019 |
url |
http://hdl.handle.net/10477/79482 https://doi.org/10.1029/2019GL082786 |
geographic |
Canada Greenland |
geographic_facet |
Canada Greenland |
genre |
East Greenland glacier glacier* Greenland Ice Sheet |
genre_facet |
East Greenland glacier glacier* Greenland Ice Sheet |
op_relation |
Datasets associated with article: http://hdl.handle.net/10477/79241 doi:10.1029/2019GL082786 Poinar, K., Dow, C.F., and Andrews, L.C. (2019). Long-term support of an active subglacial hydrologic system in Southeast Greenland by firn aquifers. Geophysical Research Letters, https://doi.org/10.1029/2019GL082786 http://hdl.handle.net/10477/79482 |
op_rights |
An edited version of this paper was published by AGU in Geophysical Research Letters. Copyright (2019) American Geophysical Union. Further reproduction or electronic distribution is not permitted. American Geophysical Union |
op_doi |
https://doi.org/10.1029/2019GL082786 |
container_title |
Geophysical Research Letters |
container_volume |
46 |
container_issue |
9 |
container_start_page |
4772 |
op_container_end_page |
4781 |
_version_ |
1766399647887130624 |