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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2021
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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 |
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15 |
container_issue |
2 |
container_start_page |
663 |
op_container_end_page |
676 |
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1766138393766395904 |