Brief communication: The Impact of Interannual Melt Supply Variability on Greenland Ice Sheet Moulin Inputs
The supraglacial drainage system of the Greenland Ice Sheet, in combination with surface melt rate, controls the rate of water flow into moulins, driving subglacial water pressure. We apply a physically-based surface meltwater flow model to a ∼20 × 27 km 2 catchment on the southwestern Greenland Ice...
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ftcopernicus:oai:publications.copernicus.org:tcd106213 2023-05-15T16:25:01+02:00 Brief communication: The Impact of Interannual Melt Supply Variability on Greenland Ice Sheet Moulin Inputs Hill, Tim Dow, Christine F. 2022-10-27 application/pdf https://doi.org/10.5194/tc-2022-180 https://tc.copernicus.org/preprints/tc-2022-180/ eng eng doi:10.5194/tc-2022-180 https://tc.copernicus.org/preprints/tc-2022-180/ eISSN: 1994-0424 Text 2022 ftcopernicus https://doi.org/10.5194/tc-2022-180 2022-10-31T17:22:43Z The supraglacial drainage system of the Greenland Ice Sheet, in combination with surface melt rate, controls the rate of water flow into moulins, driving subglacial water pressure. We apply a physically-based surface meltwater flow model to a ∼20 × 27 km 2 catchment on the southwestern Greenland Ice Sheet in high and low melt years to examine the impact of surface melt rate and variability on moulin inputs. The model outputs predict important differences in moulin inputs between high and low melt years. These dynamic model outputs will be important in driving future process-scale subglacial hydrology models. Text Greenland Ice Sheet Copernicus Publications: E-Journals Greenland |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
The supraglacial drainage system of the Greenland Ice Sheet, in combination with surface melt rate, controls the rate of water flow into moulins, driving subglacial water pressure. We apply a physically-based surface meltwater flow model to a ∼20 × 27 km 2 catchment on the southwestern Greenland Ice Sheet in high and low melt years to examine the impact of surface melt rate and variability on moulin inputs. The model outputs predict important differences in moulin inputs between high and low melt years. These dynamic model outputs will be important in driving future process-scale subglacial hydrology models. |
format |
Text |
author |
Hill, Tim Dow, Christine F. |
spellingShingle |
Hill, Tim Dow, Christine F. Brief communication: The Impact of Interannual Melt Supply Variability on Greenland Ice Sheet Moulin Inputs |
author_facet |
Hill, Tim Dow, Christine F. |
author_sort |
Hill, Tim |
title |
Brief communication: The Impact of Interannual Melt Supply Variability on Greenland Ice Sheet Moulin Inputs |
title_short |
Brief communication: The Impact of Interannual Melt Supply Variability on Greenland Ice Sheet Moulin Inputs |
title_full |
Brief communication: The Impact of Interannual Melt Supply Variability on Greenland Ice Sheet Moulin Inputs |
title_fullStr |
Brief communication: The Impact of Interannual Melt Supply Variability on Greenland Ice Sheet Moulin Inputs |
title_full_unstemmed |
Brief communication: The Impact of Interannual Melt Supply Variability on Greenland Ice Sheet Moulin Inputs |
title_sort |
brief communication: the impact of interannual melt supply variability on greenland ice sheet moulin inputs |
publishDate |
2022 |
url |
https://doi.org/10.5194/tc-2022-180 https://tc.copernicus.org/preprints/tc-2022-180/ |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Ice Sheet |
genre_facet |
Greenland Ice Sheet |
op_source |
eISSN: 1994-0424 |
op_relation |
doi:10.5194/tc-2022-180 https://tc.copernicus.org/preprints/tc-2022-180/ |
op_doi |
https://doi.org/10.5194/tc-2022-180 |
_version_ |
1766013649703403520 |