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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Main Authors: Hill, Tim, Dow, Christine F.
Format: Text
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.5194/tc-2022-180
https://tc.copernicus.org/preprints/tc-2022-180/
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spelling 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
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id 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
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