Glacier change in the Cariboo Mountains, British Columbia, Canada (1952–2005)

We applied photogrammetric methods with aerial photography from 11 different years between 1946 and 2005 to assess changes in area and volume of 33 glaciers in the Cariboo Mountains of British Columbia for the latter half of the 20th century. These are used to identify changes in extent and elevatio...

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Main Authors: M. J. Beedle, B. Menounos, R. Wheate
Format: Article
Language:English
Published: Copernicus Publications 2015-01-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/9/65/2015/tc-9-65-2015.pdf
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spelling doaj-c58e029a977e400c99028296d3b3ec902020-11-24T23:38:56ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242015-01-0191658010.5194/tc-9-65-2015Glacier change in the Cariboo Mountains, British Columbia, Canada (1952&ndash;2005)M. J. Beedle0B. Menounos1R. Wheate2Geography Program, University of Northern British Columbia, Prince George, BC, CanadaGeography Program, University of Northern British Columbia, Prince George, BC, CanadaGeography Program, University of Northern British Columbia, Prince George, BC, CanadaWe applied photogrammetric methods with aerial photography from 11 different years between 1946 and 2005 to assess changes in area and volume of 33 glaciers in the Cariboo Mountains of British Columbia for the latter half of the 20th century. These are used to identify changes in extent and elevation primarily for the periods 1952–1985, 1985–2005, and 1952–2005. All glaciers receded during the period 1952–2005; area retreat averaged −0.19 ± 0.05 % a<sup>−1</sup>. From 1952 to 1985, nine glaciers advanced; following 1985, retreat rates accelerated to −0.41 ± 0.12% a<sup>−1</sup>. Thinning rates of a subset of seven glaciers likewise accelerated, from −0.14 ± 0.04 m w.e. a<sup>−1</sup> (1952–1985) to −0.50 ± 0.07 m w.e. a<sup>−1</sup> for the period 1985–2005. Temperatures increased from the earlier to the latter period for the ablation (+0.38 °C) and accumulation (+0.87 °C) seasons, and average precipitation decreased, particularly in the accumulation season (−32 mm, −3.2%). Our comparison of surface area change with glacier morphometry corroborates previous studies that show primary relations between extent change and surface area. We also find that the strength and sign of these relations varied for different epochs. Our results also indicate that the 1985 glacier extent for the study area reported previously by other studies may be slightly overestimated due to errant mapping of late-lying snow cover.http://www.the-cryosphere.net/9/65/2015/tc-9-65-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. J. Beedle
B. Menounos
R. Wheate
spellingShingle M. J. Beedle
B. Menounos
R. Wheate
Glacier change in the Cariboo Mountains, British Columbia, Canada (1952&ndash;2005)
The Cryosphere
author_facet M. J. Beedle
B. Menounos
R. Wheate
author_sort M. J. Beedle
title Glacier change in the Cariboo Mountains, British Columbia, Canada (1952&ndash;2005)
title_short Glacier change in the Cariboo Mountains, British Columbia, Canada (1952&ndash;2005)
title_full Glacier change in the Cariboo Mountains, British Columbia, Canada (1952&ndash;2005)
title_fullStr Glacier change in the Cariboo Mountains, British Columbia, Canada (1952&ndash;2005)
title_full_unstemmed Glacier change in the Cariboo Mountains, British Columbia, Canada (1952&ndash;2005)
title_sort glacier change in the cariboo mountains, british columbia, canada (1952&ndash;2005)
publisher Copernicus Publications
series The Cryosphere
issn 1994-0416
1994-0424
publishDate 2015-01-01
description We applied photogrammetric methods with aerial photography from 11 different years between 1946 and 2005 to assess changes in area and volume of 33 glaciers in the Cariboo Mountains of British Columbia for the latter half of the 20th century. These are used to identify changes in extent and elevation primarily for the periods 1952–1985, 1985–2005, and 1952–2005. All glaciers receded during the period 1952–2005; area retreat averaged −0.19 ± 0.05 % a<sup>−1</sup>. From 1952 to 1985, nine glaciers advanced; following 1985, retreat rates accelerated to −0.41 ± 0.12% a<sup>−1</sup>. Thinning rates of a subset of seven glaciers likewise accelerated, from −0.14 ± 0.04 m w.e. a<sup>−1</sup> (1952–1985) to −0.50 ± 0.07 m w.e. a<sup>−1</sup> for the period 1985–2005. Temperatures increased from the earlier to the latter period for the ablation (+0.38 °C) and accumulation (+0.87 °C) seasons, and average precipitation decreased, particularly in the accumulation season (−32 mm, −3.2%). Our comparison of surface area change with glacier morphometry corroborates previous studies that show primary relations between extent change and surface area. We also find that the strength and sign of these relations varied for different epochs. Our results also indicate that the 1985 glacier extent for the study area reported previously by other studies may be slightly overestimated due to errant mapping of late-lying snow cover.
url http://www.the-cryosphere.net/9/65/2015/tc-9-65-2015.pdf
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