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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Main Authors: Bunce, C., Nienow, P., Sole, A., Cowton, T., Davison, B.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2021
Subjects:
Online Access:https://eprints.whiterose.ac.uk/170546/
https://eprints.whiterose.ac.uk/170546/1/Bunce%20et%20al%202020%20Influence%20of%20glacier%20runoff%20and%20near-terminus%20subglacial%20hydrology%20on%20frontal%20ablation%20at%20a%20large%20Greenlandic%20tidewater%20glacier.pdf
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record_format openpolar
spelling ftleedsuniv:oai:eprints.whiterose.ac.uk:170546 2023-05-15T16:21:14+02:00 Influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large Greenlandic tidewater glacier Bunce, C. Nienow, P. Sole, A. Cowton, T. Davison, B. 2021-04 text https://eprints.whiterose.ac.uk/170546/ https://eprints.whiterose.ac.uk/170546/1/Bunce%20et%20al%202020%20Influence%20of%20glacier%20runoff%20and%20near-terminus%20subglacial%20hydrology%20on%20frontal%20ablation%20at%20a%20large%20Greenlandic%20tidewater%20glacier.pdf en eng Cambridge University Press (CUP) https://eprints.whiterose.ac.uk/170546/1/Bunce%20et%20al%202020%20Influence%20of%20glacier%20runoff%20and%20near-terminus%20subglacial%20hydrology%20on%20frontal%20ablation%20at%20a%20large%20Greenlandic%20tidewater%20glacier.pdf Bunce, C., Nienow, P., Sole, A. orcid.org/0000-0001-5290-8967 et al. (2 more authors) (2021) Influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large Greenlandic tidewater glacier. Journal of Glaciology, 67 (262). pp. 343-352. ISSN 0022-1430 cc_by_4 CC-BY Article PeerReviewed 2021 ftleedsuniv 2023-01-30T22:36:13Z 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 glacier Greenland greenlandic Ice Sheet Journal of Glaciology Tidewater White Rose Research Online (Universities of Leeds, Sheffield & York) Greenland
institution Open Polar
collection White Rose Research Online (Universities of Leeds, Sheffield & York)
op_collection_id ftleedsuniv
language English
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 Bunce, C.
Nienow, P.
Sole, A.
Cowton, T.
Davison, B.
spellingShingle Bunce, C.
Nienow, P.
Sole, A.
Cowton, T.
Davison, B.
Influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large Greenlandic tidewater glacier
author_facet Bunce, C.
Nienow, P.
Sole, A.
Cowton, T.
Davison, B.
author_sort Bunce, C.
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 (CUP)
publishDate 2021
url https://eprints.whiterose.ac.uk/170546/
https://eprints.whiterose.ac.uk/170546/1/Bunce%20et%20al%202020%20Influence%20of%20glacier%20runoff%20and%20near-terminus%20subglacial%20hydrology%20on%20frontal%20ablation%20at%20a%20large%20Greenlandic%20tidewater%20glacier.pdf
geographic Greenland
geographic_facet Greenland
genre glacier
Greenland
greenlandic
Ice Sheet
Journal of Glaciology
Tidewater
genre_facet glacier
Greenland
greenlandic
Ice Sheet
Journal of Glaciology
Tidewater
op_relation https://eprints.whiterose.ac.uk/170546/1/Bunce%20et%20al%202020%20Influence%20of%20glacier%20runoff%20and%20near-terminus%20subglacial%20hydrology%20on%20frontal%20ablation%20at%20a%20large%20Greenlandic%20tidewater%20glacier.pdf
Bunce, C., Nienow, P., Sole, A. orcid.org/0000-0001-5290-8967 et al. (2 more authors) (2021) Influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large Greenlandic tidewater glacier. Journal of Glaciology, 67 (262). pp. 343-352. ISSN 0022-1430
op_rights cc_by_4
op_rightsnorm CC-BY
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