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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Cambridge University Press
2021
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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 |
_version_ |
1766339421365338112 |