Influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large Greenlandic tidewater glacier

Frontal ablation from tidewater glaciers is a major component of the total mass loss from the Greenland ice sheet. It remains unclear, however, how changes in atmospheric and oceanic temperatures translate into changes in frontal ablation, in part due to sparse observations at sufficiently high spat...

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Published in:Journal of Glaciology
Main Authors: Charlie Bunce, Peter Nienow, Andrew Sole, Tom Cowton, Benjamin Davison
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2021
Subjects:
Online Access:https://doi.org/10.1017/jog.2020.109
https://doaj.org/article/6f8a8edf9eec4d46aec097473ab11929
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spelling ftdoajarticles:oai:doaj.org/article:6f8a8edf9eec4d46aec097473ab11929 2023-05-15T15:07:59+02:00 Influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large Greenlandic tidewater glacier Charlie Bunce Peter Nienow Andrew Sole Tom Cowton Benjamin Davison 2021-04-01T00:00:00Z https://doi.org/10.1017/jog.2020.109 https://doaj.org/article/6f8a8edf9eec4d46aec097473ab11929 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143020001094/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2020.109 0022-1430 1727-5652 https://doaj.org/article/6f8a8edf9eec4d46aec097473ab11929 Journal of Glaciology, Vol 67, Pp 343-352 (2021) Arctic glaciology ice/ocean interactions iceberg calving Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2021 ftdoajarticles https://doi.org/10.1017/jog.2020.109 2023-03-12T01:30:57Z Frontal ablation from tidewater glaciers is a major component of the total mass loss from the Greenland ice sheet. It remains unclear, however, how changes in atmospheric and oceanic temperatures translate into changes in frontal ablation, in part due to sparse observations at sufficiently high spatial and temporal resolution. We present high-frequency time-lapse imagery (photos every 30 min) of iceberg calving and meltwater plumes at Kangiata Nunaata Sermia (KNS), southwest Greenland, during June–October 2017, alongside satellite-derived ice velocities and modelled subglacial discharge. Early in the melt season, we infer a subglacial hydrological network with multiple outlets that would theoretically distribute discharge and enhance undercutting by submarine melt, an inference supported by our observations of terminus-wide calving during this period. During the melt season, we infer hydraulic evolution to a relatively more channelised subglacial drainage configuration, based on meltwater plume visibility indicating focused emergence of subglacial water; these observations coincide with a reduction in terminus-wide calving and transition to an incised planform terminus geometry. We suggest that temporal variations in subglacial discharge and near-terminus subglacial hydraulic efficiency exert considerable influence on calving and frontal ablation at KNS. Article in Journal/Newspaper Arctic glacier Greenland greenlandic Ice Sheet Iceberg* Journal of Glaciology Tidewater Directory of Open Access Journals: DOAJ Articles Arctic Greenland Journal of Glaciology 67 262 343 352
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Arctic glaciology
ice/ocean interactions
iceberg calving
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Arctic glaciology
ice/ocean interactions
iceberg calving
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Charlie Bunce
Peter Nienow
Andrew Sole
Tom Cowton
Benjamin Davison
Influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large Greenlandic tidewater glacier
topic_facet Arctic glaciology
ice/ocean interactions
iceberg calving
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Frontal ablation from tidewater glaciers is a major component of the total mass loss from the Greenland ice sheet. It remains unclear, however, how changes in atmospheric and oceanic temperatures translate into changes in frontal ablation, in part due to sparse observations at sufficiently high spatial and temporal resolution. We present high-frequency time-lapse imagery (photos every 30 min) of iceberg calving and meltwater plumes at Kangiata Nunaata Sermia (KNS), southwest Greenland, during June–October 2017, alongside satellite-derived ice velocities and modelled subglacial discharge. Early in the melt season, we infer a subglacial hydrological network with multiple outlets that would theoretically distribute discharge and enhance undercutting by submarine melt, an inference supported by our observations of terminus-wide calving during this period. During the melt season, we infer hydraulic evolution to a relatively more channelised subglacial drainage configuration, based on meltwater plume visibility indicating focused emergence of subglacial water; these observations coincide with a reduction in terminus-wide calving and transition to an incised planform terminus geometry. We suggest that temporal variations in subglacial discharge and near-terminus subglacial hydraulic efficiency exert considerable influence on calving and frontal ablation at KNS.
format Article in Journal/Newspaper
author Charlie Bunce
Peter Nienow
Andrew Sole
Tom Cowton
Benjamin Davison
author_facet Charlie Bunce
Peter Nienow
Andrew Sole
Tom Cowton
Benjamin Davison
author_sort Charlie Bunce
title Influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large Greenlandic tidewater glacier
title_short Influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large Greenlandic tidewater glacier
title_full Influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large Greenlandic tidewater glacier
title_fullStr Influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large Greenlandic tidewater glacier
title_full_unstemmed Influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large Greenlandic tidewater glacier
title_sort influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large greenlandic tidewater glacier
publisher Cambridge University Press
publishDate 2021
url https://doi.org/10.1017/jog.2020.109
https://doaj.org/article/6f8a8edf9eec4d46aec097473ab11929
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
glacier
Greenland
greenlandic
Ice Sheet
Iceberg*
Journal of Glaciology
Tidewater
genre_facet Arctic
glacier
Greenland
greenlandic
Ice Sheet
Iceberg*
Journal of Glaciology
Tidewater
op_source Journal of Glaciology, Vol 67, Pp 343-352 (2021)
op_relation https://www.cambridge.org/core/product/identifier/S0022143020001094/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2020.109
0022-1430
1727-5652
https://doaj.org/article/6f8a8edf9eec4d46aec097473ab11929
op_doi https://doi.org/10.1017/jog.2020.109
container_title Journal of Glaciology
container_volume 67
container_issue 262
container_start_page 343
op_container_end_page 352
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