Persistent overcut regions dominate the terminus morphology of a rapidly melting tidewater glacier
Frontal ablation, the combination of submarine melting and iceberg calving, changes the geometry of a glacier's terminus, influencing glacier dynamics, the fate of upwelling plumes and the distribution of submarine meltwater input into the ocean. Directly observing frontal ablation and terminus...
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Cambridge University Press
2023
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Online Access: | https://doi.org/10.1017/aog.2023.38 https://doaj.org/article/8a724f67bdcd4b6bb16595b09e827016 |
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ftdoajarticles:oai:doaj.org/article:8a724f67bdcd4b6bb16595b09e827016 2024-09-15T17:39:55+00:00 Persistent overcut regions dominate the terminus morphology of a rapidly melting tidewater glacier Nicole Abib David A. Sutherland Jason M. Amundson Dan Duncan Emily F. Eidam Rebecca H. Jackson Christian Kienholz Mathieu Morlighem Roman J. Motyka Jonathan D. Nash Bridget Ovall Erin C. Pettit 2023-04-01T00:00:00Z https://doi.org/10.1017/aog.2023.38 https://doaj.org/article/8a724f67bdcd4b6bb16595b09e827016 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0260305523000381/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2023.38 0260-3055 1727-5644 https://doaj.org/article/8a724f67bdcd4b6bb16595b09e827016 Annals of Glaciology, Vol 64, Pp 1-12 (2023) Glacier ablation phenomena ice/ocean interactions iceberg calving Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1017/aog.2023.38 2024-08-05T17:49:57Z Frontal ablation, the combination of submarine melting and iceberg calving, changes the geometry of a glacier's terminus, influencing glacier dynamics, the fate of upwelling plumes and the distribution of submarine meltwater input into the ocean. Directly observing frontal ablation and terminus morphology below the waterline is difficult, however, limiting our understanding of these coupled ice–ocean processes. To investigate the evolution of a tidewater glacier's submarine terminus, we combine 3-D multibeam point clouds of the subsurface ice face at LeConte Glacier, Alaska, with concurrent observations of environmental conditions during three field campaigns between 2016 and 2018. We observe terminus morphology that was predominately overcut (52% in August 2016, 63% in May 2017 and 74% in September 2018), accompanied by high multibeam sonar-derived melt rates (4.84 m d−1 in 2016, 1.13 m d−1 in 2017 and 1.85 m d−1 in 2018). We find that periods of high subglacial discharge lead to localized undercut discharge outlets, but adjacent to these outlets the terminus maintains significantly overcut geometry, with an ice ramp that protrudes 75 m into the fjord in 2017 and 125 m in 2018. Our data challenge the assumption that tidewater glacier termini are largely undercut during periods of high submarine melting. Article in Journal/Newspaper Annals of Glaciology glacier Tidewater Alaska Directory of Open Access Journals: DOAJ Articles Annals of Glaciology 1 12 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Glacier ablation phenomena ice/ocean interactions iceberg calving Meteorology. Climatology QC851-999 |
spellingShingle |
Glacier ablation phenomena ice/ocean interactions iceberg calving Meteorology. Climatology QC851-999 Nicole Abib David A. Sutherland Jason M. Amundson Dan Duncan Emily F. Eidam Rebecca H. Jackson Christian Kienholz Mathieu Morlighem Roman J. Motyka Jonathan D. Nash Bridget Ovall Erin C. Pettit Persistent overcut regions dominate the terminus morphology of a rapidly melting tidewater glacier |
topic_facet |
Glacier ablation phenomena ice/ocean interactions iceberg calving Meteorology. Climatology QC851-999 |
description |
Frontal ablation, the combination of submarine melting and iceberg calving, changes the geometry of a glacier's terminus, influencing glacier dynamics, the fate of upwelling plumes and the distribution of submarine meltwater input into the ocean. Directly observing frontal ablation and terminus morphology below the waterline is difficult, however, limiting our understanding of these coupled ice–ocean processes. To investigate the evolution of a tidewater glacier's submarine terminus, we combine 3-D multibeam point clouds of the subsurface ice face at LeConte Glacier, Alaska, with concurrent observations of environmental conditions during three field campaigns between 2016 and 2018. We observe terminus morphology that was predominately overcut (52% in August 2016, 63% in May 2017 and 74% in September 2018), accompanied by high multibeam sonar-derived melt rates (4.84 m d−1 in 2016, 1.13 m d−1 in 2017 and 1.85 m d−1 in 2018). We find that periods of high subglacial discharge lead to localized undercut discharge outlets, but adjacent to these outlets the terminus maintains significantly overcut geometry, with an ice ramp that protrudes 75 m into the fjord in 2017 and 125 m in 2018. Our data challenge the assumption that tidewater glacier termini are largely undercut during periods of high submarine melting. |
format |
Article in Journal/Newspaper |
author |
Nicole Abib David A. Sutherland Jason M. Amundson Dan Duncan Emily F. Eidam Rebecca H. Jackson Christian Kienholz Mathieu Morlighem Roman J. Motyka Jonathan D. Nash Bridget Ovall Erin C. Pettit |
author_facet |
Nicole Abib David A. Sutherland Jason M. Amundson Dan Duncan Emily F. Eidam Rebecca H. Jackson Christian Kienholz Mathieu Morlighem Roman J. Motyka Jonathan D. Nash Bridget Ovall Erin C. Pettit |
author_sort |
Nicole Abib |
title |
Persistent overcut regions dominate the terminus morphology of a rapidly melting tidewater glacier |
title_short |
Persistent overcut regions dominate the terminus morphology of a rapidly melting tidewater glacier |
title_full |
Persistent overcut regions dominate the terminus morphology of a rapidly melting tidewater glacier |
title_fullStr |
Persistent overcut regions dominate the terminus morphology of a rapidly melting tidewater glacier |
title_full_unstemmed |
Persistent overcut regions dominate the terminus morphology of a rapidly melting tidewater glacier |
title_sort |
persistent overcut regions dominate the terminus morphology of a rapidly melting tidewater glacier |
publisher |
Cambridge University Press |
publishDate |
2023 |
url |
https://doi.org/10.1017/aog.2023.38 https://doaj.org/article/8a724f67bdcd4b6bb16595b09e827016 |
genre |
Annals of Glaciology glacier Tidewater Alaska |
genre_facet |
Annals of Glaciology glacier Tidewater Alaska |
op_source |
Annals of Glaciology, Vol 64, Pp 1-12 (2023) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0260305523000381/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2023.38 0260-3055 1727-5644 https://doaj.org/article/8a724f67bdcd4b6bb16595b09e827016 |
op_doi |
https://doi.org/10.1017/aog.2023.38 |
container_title |
Annals of Glaciology |
container_start_page |
1 |
op_container_end_page |
12 |
_version_ |
1810483465955573760 |