Retreat of Glaciar Tyndall, Patagonia, over the last half-century
We report measurements of ice surface elevation, ice thickness and surface area for Glaciar Tyndall, Patagonia, made in 1999-2002. The measurements, together with previously published observations, show acceleration over the last few decades of the rates of thinning and retreat of the main calving f...
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Language: | English |
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2005
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ftcdlib:qt2dj4h5qm 2023-05-15T16:57:38+02:00 Retreat of Glaciar Tyndall, Patagonia, over the last half-century Raymond, C Neumann, TA Rignot, E Echelmeyer, K Rivera, A Casassa, G 239 - 247 2005-01-01 application/pdf http://www.escholarship.org/uc/item/2dj4h5qm english eng eScholarship, University of California qt2dj4h5qm http://www.escholarship.org/uc/item/2dj4h5qm Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ CC-BY Raymond, C; Neumann, TA; Rignot, E; Echelmeyer, K; Rivera, A; & Casassa, G. (2005). Retreat of Glaciar Tyndall, Patagonia, over the last half-century. Journal of Glaciology, 51(173), 239 - 247. doi:10.3189/172756505781829476. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/2dj4h5qm article 2005 ftcdlib https://doi.org/10.3189/172756505781829476 2018-07-06T22:51:35Z We report measurements of ice surface elevation, ice thickness and surface area for Glaciar Tyndall, Patagonia, made in 1999-2002. The measurements, together with previously published observations, show acceleration over the last few decades of the rates of thinning and retreat of the main calving front. The acceleration of shrinkage appears to be driven by a combination of climate and feedback processes, the dominant feedback being increased melting associated with lowering of the glacier surface (elevation feedback). The melting capacity in the main terminus lake is now too small to be a major factor accelerating the retreat. The glacier bed has low slope and remains below the elevation of the lake spillway for >14 km upstream from the 2000 calving front, indicating the potential for extensive retreat under the influence of strong elevation feedback and increasing interaction with the lake as it enlarges. Article in Journal/Newspaper Journal of Glaciology University of California: eScholarship Patagonia Journal of Glaciology 51 173 239 247 |
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Open Polar |
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University of California: eScholarship |
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ftcdlib |
language |
English |
description |
We report measurements of ice surface elevation, ice thickness and surface area for Glaciar Tyndall, Patagonia, made in 1999-2002. The measurements, together with previously published observations, show acceleration over the last few decades of the rates of thinning and retreat of the main calving front. The acceleration of shrinkage appears to be driven by a combination of climate and feedback processes, the dominant feedback being increased melting associated with lowering of the glacier surface (elevation feedback). The melting capacity in the main terminus lake is now too small to be a major factor accelerating the retreat. The glacier bed has low slope and remains below the elevation of the lake spillway for >14 km upstream from the 2000 calving front, indicating the potential for extensive retreat under the influence of strong elevation feedback and increasing interaction with the lake as it enlarges. |
format |
Article in Journal/Newspaper |
author |
Raymond, C Neumann, TA Rignot, E Echelmeyer, K Rivera, A Casassa, G |
spellingShingle |
Raymond, C Neumann, TA Rignot, E Echelmeyer, K Rivera, A Casassa, G Retreat of Glaciar Tyndall, Patagonia, over the last half-century |
author_facet |
Raymond, C Neumann, TA Rignot, E Echelmeyer, K Rivera, A Casassa, G |
author_sort |
Raymond, C |
title |
Retreat of Glaciar Tyndall, Patagonia, over the last half-century |
title_short |
Retreat of Glaciar Tyndall, Patagonia, over the last half-century |
title_full |
Retreat of Glaciar Tyndall, Patagonia, over the last half-century |
title_fullStr |
Retreat of Glaciar Tyndall, Patagonia, over the last half-century |
title_full_unstemmed |
Retreat of Glaciar Tyndall, Patagonia, over the last half-century |
title_sort |
retreat of glaciar tyndall, patagonia, over the last half-century |
publisher |
eScholarship, University of California |
publishDate |
2005 |
url |
http://www.escholarship.org/uc/item/2dj4h5qm |
op_coverage |
239 - 247 |
geographic |
Patagonia |
geographic_facet |
Patagonia |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Raymond, C; Neumann, TA; Rignot, E; Echelmeyer, K; Rivera, A; & Casassa, G. (2005). Retreat of Glaciar Tyndall, Patagonia, over the last half-century. Journal of Glaciology, 51(173), 239 - 247. doi:10.3189/172756505781829476. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/2dj4h5qm |
op_relation |
qt2dj4h5qm http://www.escholarship.org/uc/item/2dj4h5qm |
op_rights |
Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.3189/172756505781829476 |
container_title |
Journal of Glaciology |
container_volume |
51 |
container_issue |
173 |
container_start_page |
239 |
op_container_end_page |
247 |
_version_ |
1766049196264128512 |