Recent acceleration of Denman Glacier (1972–2017), East Antarctica, driven by grounding line retreat and changes in ice tongue configuration

After Totten, Denman Glacier is the largest contributor to sea level rise in East Antarctica. Denman's catchment contains an ice volume equivalent to 1.5 m of global sea level and sits in the Aurora Subglacial Basin (ASB). Geological evidence of this basin's sensitivity to past warm period...

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Published in:The Cryosphere
Main Authors: B. W. J. Miles, J. R. Jordan, C. R. Stokes, S. S. R. Jamieson, G. H. Gudmundsson, A. Jenkins
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2021
Subjects:
Online Access:https://doi.org/10.5194/tc-15-663-2021
https://doaj.org/article/35c3f50e118b4e299c3c4f9d2e98cc01
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spelling ftdoajarticles:oai:doaj.org/article:35c3f50e118b4e299c3c4f9d2e98cc01 2023-05-15T13:40:41+02:00 Recent acceleration of Denman Glacier (1972–2017), East Antarctica, driven by grounding line retreat and changes in ice tongue configuration B. W. J. Miles J. R. Jordan C. R. Stokes S. S. R. Jamieson G. H. Gudmundsson A. Jenkins 2021-02-01T00:00:00Z https://doi.org/10.5194/tc-15-663-2021 https://doaj.org/article/35c3f50e118b4e299c3c4f9d2e98cc01 EN eng Copernicus Publications https://tc.copernicus.org/articles/15/663/2021/tc-15-663-2021.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-15-663-2021 1994-0416 1994-0424 https://doaj.org/article/35c3f50e118b4e299c3c4f9d2e98cc01 The Cryosphere, Vol 15, Pp 663-676 (2021) Environmental sciences GE1-350 Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.5194/tc-15-663-2021 2022-12-31T04:38:29Z After Totten, Denman Glacier is the largest contributor to sea level rise in East Antarctica. Denman's catchment contains an ice volume equivalent to 1.5 m of global sea level and sits in the Aurora Subglacial Basin (ASB). Geological evidence of this basin's sensitivity to past warm periods, combined with recent observations showing that Denman's ice speed is accelerating and its grounding line is retreating along a retrograde slope, has raised the prospect that its contributions to sea level rise could accelerate. In this study, we produce the first long-term ( ∼50 years) record of past glacier behaviour (ice flow speed, ice tongue structure and calving) and combine these observations with numerical modelling to explore the likely drivers of its recent change. We find a spatially widespread acceleration of the Denman system since the 1970s across both its grounded ( 17±4 % acceleration; 1972–2017) and floating portions ( 36±5 % acceleration; 1972–2017). Our numerical modelling experiments show that a combination of grounding line retreat, ice tongue thinning and the unpinning of Denman's ice tongue from a pinning point following its last major calving event are required to simulate an acceleration comparable with observations. Given its bed topography and the geological evidence that Denman Glacier has retreated substantially in the past, its recent grounding line retreat and ice flow acceleration suggest that it could be poised to make a significant contribution to sea level in the near future. Article in Journal/Newspaper Antarc* Antarctica Denman Glacier East Antarctica The Cryosphere Directory of Open Access Journals: DOAJ Articles East Antarctica Denman Glacier ENVELOPE(99.417,99.417,-66.750,-66.750) The Cryosphere 15 2 663 676
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
B. W. J. Miles
J. R. Jordan
C. R. Stokes
S. S. R. Jamieson
G. H. Gudmundsson
A. Jenkins
Recent acceleration of Denman Glacier (1972–2017), East Antarctica, driven by grounding line retreat and changes in ice tongue configuration
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description After Totten, Denman Glacier is the largest contributor to sea level rise in East Antarctica. Denman's catchment contains an ice volume equivalent to 1.5 m of global sea level and sits in the Aurora Subglacial Basin (ASB). Geological evidence of this basin's sensitivity to past warm periods, combined with recent observations showing that Denman's ice speed is accelerating and its grounding line is retreating along a retrograde slope, has raised the prospect that its contributions to sea level rise could accelerate. In this study, we produce the first long-term ( ∼50 years) record of past glacier behaviour (ice flow speed, ice tongue structure and calving) and combine these observations with numerical modelling to explore the likely drivers of its recent change. We find a spatially widespread acceleration of the Denman system since the 1970s across both its grounded ( 17±4 % acceleration; 1972–2017) and floating portions ( 36±5 % acceleration; 1972–2017). Our numerical modelling experiments show that a combination of grounding line retreat, ice tongue thinning and the unpinning of Denman's ice tongue from a pinning point following its last major calving event are required to simulate an acceleration comparable with observations. Given its bed topography and the geological evidence that Denman Glacier has retreated substantially in the past, its recent grounding line retreat and ice flow acceleration suggest that it could be poised to make a significant contribution to sea level in the near future.
format Article in Journal/Newspaper
author B. W. J. Miles
J. R. Jordan
C. R. Stokes
S. S. R. Jamieson
G. H. Gudmundsson
A. Jenkins
author_facet B. W. J. Miles
J. R. Jordan
C. R. Stokes
S. S. R. Jamieson
G. H. Gudmundsson
A. Jenkins
author_sort B. W. J. Miles
title Recent acceleration of Denman Glacier (1972–2017), East Antarctica, driven by grounding line retreat and changes in ice tongue configuration
title_short Recent acceleration of Denman Glacier (1972–2017), East Antarctica, driven by grounding line retreat and changes in ice tongue configuration
title_full Recent acceleration of Denman Glacier (1972–2017), East Antarctica, driven by grounding line retreat and changes in ice tongue configuration
title_fullStr Recent acceleration of Denman Glacier (1972–2017), East Antarctica, driven by grounding line retreat and changes in ice tongue configuration
title_full_unstemmed Recent acceleration of Denman Glacier (1972–2017), East Antarctica, driven by grounding line retreat and changes in ice tongue configuration
title_sort recent acceleration of denman glacier (1972–2017), east antarctica, driven by grounding line retreat and changes in ice tongue configuration
publisher Copernicus Publications
publishDate 2021
url https://doi.org/10.5194/tc-15-663-2021
https://doaj.org/article/35c3f50e118b4e299c3c4f9d2e98cc01
long_lat ENVELOPE(99.417,99.417,-66.750,-66.750)
geographic East Antarctica
Denman Glacier
geographic_facet East Antarctica
Denman Glacier
genre Antarc*
Antarctica
Denman Glacier
East Antarctica
The Cryosphere
genre_facet Antarc*
Antarctica
Denman Glacier
East Antarctica
The Cryosphere
op_source The Cryosphere, Vol 15, Pp 663-676 (2021)
op_relation https://tc.copernicus.org/articles/15/663/2021/tc-15-663-2021.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-15-663-2021
1994-0416
1994-0424
https://doaj.org/article/35c3f50e118b4e299c3c4f9d2e98cc01
op_doi https://doi.org/10.5194/tc-15-663-2021
container_title The Cryosphere
container_volume 15
container_issue 2
container_start_page 663
op_container_end_page 676
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