‘Detachment’ of icefield outlet glaciers – catastrophic thinning and retreat of the Columbia Glacier (Canada)
We present an investigation of changes taking place on the Columbia Glacier – a lake-terminating outlet of the Columbia Icefield in the Canadian Rockies. The Columbia Icefield is the largest, and one of the most important, ice bodies in the Canadian Rockies. Like other ice masses, it stores water as...
Published in: | Earth Surface Processes and Landforms |
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ftleedsuniv:oai:eprints.whiterose.ac.uk:151285 2023-05-15T16:22:29+02:00 ‘Detachment’ of icefield outlet glaciers – catastrophic thinning and retreat of the Columbia Glacier (Canada) Rippin, David Manish Sharp, Martin Van Wychen, Wesley Zubot, Darryl 2019-10-27 text https://eprints.whiterose.ac.uk/151285/ https://eprints.whiterose.ac.uk/151285/1/Rippin_et_al_revision_author_accepted_manuscript.pdf https://doi.org/10.1002/esp.4746 en eng https://eprints.whiterose.ac.uk/151285/1/Rippin_et_al_revision_author_accepted_manuscript.pdf Rippin, David Manish orcid.org/0000-0001-7757-9880 , Sharp, Martin, Van Wychen, Wesley et al. (1 more author) (2019) ‘Detachment’ of icefield outlet glaciers – catastrophic thinning and retreat of the Columbia Glacier (Canada). EARTH SURFACE PROCESSES AND LANDFORMS. pp. 1-14. ISSN 0197-9337 Article PeerReviewed 2019 ftleedsuniv https://doi.org/10.1002/esp.4746 2023-01-30T22:22:40Z We present an investigation of changes taking place on the Columbia Glacier – a lake-terminating outlet of the Columbia Icefield in the Canadian Rockies. The Columbia Icefield is the largest, and one of the most important, ice bodies in the Canadian Rockies. Like other ice masses, it stores water as snow and ice during the winter and releases it during warmer summer months, sustaining river flows and the ecosystems that rely on them. However, the Columbia Glacier and Icefield is shrinking. We use Landsat and Sentinel-2 imagery to show that the Columbia Glacier has retreated increasingly rapidly in recent years, and suggest that this looks set to continue. Importantly, we identify a previously undocumented process that appears to be playing an important role in the retreat of this glacier. This process involves the ‘detachment’ of the glacier tongue from its accumulation area in the Columbia Icefield. This process is important because the tongue is cut off from the accumulation area and there is no replenishment of ice that melts in the glacier's ablation area by flow from upglacier. As a consequence, for a given rate of ablation, the ice in the tongue will disappear much faster than it would if the local mass loss by melting/calving was partly offset by mass input by glacier flow. Such a change would alter the relationship between rates of surface melting and rates of glacier frontal retreat. We provide evidence that detachment has already occurred elsewhere on the Columbia Icefield and that it is likely to affect other outlet glaciers in the future. Modelling studies forecast this detachment activity, which ultimately results in a smaller ‘perched’ icefield without active outlets. Article in Journal/Newspaper glacier* White Rose Research Online (Universities of Leeds, Sheffield & York) Canada Earth Surface Processes and Landforms 45 2 459 472 |
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Open Polar |
collection |
White Rose Research Online (Universities of Leeds, Sheffield & York) |
op_collection_id |
ftleedsuniv |
language |
English |
description |
We present an investigation of changes taking place on the Columbia Glacier – a lake-terminating outlet of the Columbia Icefield in the Canadian Rockies. The Columbia Icefield is the largest, and one of the most important, ice bodies in the Canadian Rockies. Like other ice masses, it stores water as snow and ice during the winter and releases it during warmer summer months, sustaining river flows and the ecosystems that rely on them. However, the Columbia Glacier and Icefield is shrinking. We use Landsat and Sentinel-2 imagery to show that the Columbia Glacier has retreated increasingly rapidly in recent years, and suggest that this looks set to continue. Importantly, we identify a previously undocumented process that appears to be playing an important role in the retreat of this glacier. This process involves the ‘detachment’ of the glacier tongue from its accumulation area in the Columbia Icefield. This process is important because the tongue is cut off from the accumulation area and there is no replenishment of ice that melts in the glacier's ablation area by flow from upglacier. As a consequence, for a given rate of ablation, the ice in the tongue will disappear much faster than it would if the local mass loss by melting/calving was partly offset by mass input by glacier flow. Such a change would alter the relationship between rates of surface melting and rates of glacier frontal retreat. We provide evidence that detachment has already occurred elsewhere on the Columbia Icefield and that it is likely to affect other outlet glaciers in the future. Modelling studies forecast this detachment activity, which ultimately results in a smaller ‘perched’ icefield without active outlets. |
format |
Article in Journal/Newspaper |
author |
Rippin, David Manish Sharp, Martin Van Wychen, Wesley Zubot, Darryl |
spellingShingle |
Rippin, David Manish Sharp, Martin Van Wychen, Wesley Zubot, Darryl ‘Detachment’ of icefield outlet glaciers – catastrophic thinning and retreat of the Columbia Glacier (Canada) |
author_facet |
Rippin, David Manish Sharp, Martin Van Wychen, Wesley Zubot, Darryl |
author_sort |
Rippin, David Manish |
title |
‘Detachment’ of icefield outlet glaciers – catastrophic thinning and retreat of the Columbia Glacier (Canada) |
title_short |
‘Detachment’ of icefield outlet glaciers – catastrophic thinning and retreat of the Columbia Glacier (Canada) |
title_full |
‘Detachment’ of icefield outlet glaciers – catastrophic thinning and retreat of the Columbia Glacier (Canada) |
title_fullStr |
‘Detachment’ of icefield outlet glaciers – catastrophic thinning and retreat of the Columbia Glacier (Canada) |
title_full_unstemmed |
‘Detachment’ of icefield outlet glaciers – catastrophic thinning and retreat of the Columbia Glacier (Canada) |
title_sort |
‘detachment’ of icefield outlet glaciers – catastrophic thinning and retreat of the columbia glacier (canada) |
publishDate |
2019 |
url |
https://eprints.whiterose.ac.uk/151285/ https://eprints.whiterose.ac.uk/151285/1/Rippin_et_al_revision_author_accepted_manuscript.pdf https://doi.org/10.1002/esp.4746 |
geographic |
Canada |
geographic_facet |
Canada |
genre |
glacier* |
genre_facet |
glacier* |
op_relation |
https://eprints.whiterose.ac.uk/151285/1/Rippin_et_al_revision_author_accepted_manuscript.pdf Rippin, David Manish orcid.org/0000-0001-7757-9880 , Sharp, Martin, Van Wychen, Wesley et al. (1 more author) (2019) ‘Detachment’ of icefield outlet glaciers – catastrophic thinning and retreat of the Columbia Glacier (Canada). EARTH SURFACE PROCESSES AND LANDFORMS. pp. 1-14. ISSN 0197-9337 |
op_doi |
https://doi.org/10.1002/esp.4746 |
container_title |
Earth Surface Processes and Landforms |
container_volume |
45 |
container_issue |
2 |
container_start_page |
459 |
op_container_end_page |
472 |
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1766010458998833152 |