Area change of glaciers in the Canadian Rocky Mountains, 1919 to 2006
Glaciers in the Canadian Rocky Mountains constitute an important freshwater resource. To enhance our understanding of the influence climate and local topography have on glacier area, large numbers of glaciers of different sizes and attributes need to be monitored over periods of many decades. We use...
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Online Access: | https://doi.org/10.5194/tc-6-1541-2012 http://www.the-cryosphere.net/6/1541/2012/tc-6-1541-2012.pdf https://doaj.org/article/cf6671264f9d4c50bf591cc002952947 |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:cf6671264f9d4c50bf591cc002952947 2023-05-15T18:32:21+02:00 Area change of glaciers in the Canadian Rocky Mountains, 1919 to 2006 C. Tennant B. Menounos R. Wheate J. J. Clague 2012-12-01 https://doi.org/10.5194/tc-6-1541-2012 http://www.the-cryosphere.net/6/1541/2012/tc-6-1541-2012.pdf https://doaj.org/article/cf6671264f9d4c50bf591cc002952947 en eng Copernicus Publications doi:10.5194/tc-6-1541-2012 1994-0416 1994-0424 http://www.the-cryosphere.net/6/1541/2012/tc-6-1541-2012.pdf https://doaj.org/article/cf6671264f9d4c50bf591cc002952947 undefined The Cryosphere, Vol 6, Iss 6, Pp 1541-1552 (2012) envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2012 fttriple https://doi.org/10.5194/tc-6-1541-2012 2023-01-22T19:16:19Z Glaciers in the Canadian Rocky Mountains constitute an important freshwater resource. To enhance our understanding of the influence climate and local topography have on glacier area, large numbers of glaciers of different sizes and attributes need to be monitored over periods of many decades. We used Interprovincial Boundary Commission Survey (IBCS) maps of the Alberta–British Columbia (BC) border (1903–1924), BC Terrain Resource Information Management (TRIM) data (1982–1987), and Landsat Thematic Mapper (TM) and Enhanced Thematic Mapper (ETM+) imagery (2000–2002 and 2006) to document planimetric changes in glacier cover in the central and southern Canadian Rocky Mountains between 1919 and 2006. Over this period, glacier cover in the study area decreased by 590 ± 70 km2 (40 ± 5%), 17 of 523 glaciers disappeared and 124 glaciers fragmented into multiple ice masses. Glaciers smaller than 1.0 km2 experienced the greatest relative area loss (64 ± 8%), and relative area loss is more variable with small glaciers, suggesting that the local topographic setting controls the response of these glaciers to climate change. Small glaciers with low slopes, low mean/median elevations, south to west aspects, and high insolation experienced the largest reduction in area. Similar rates of area change characterize the periods 1919–1985 and 1985–2001; −6.3 ± 0.6 km2 yr−1 (−0.4 ± 0.1% yr−1) and −5.0 ± 0.5 km2 yr−1 (−0.5 ± 0.1% yr−1), respectively. The rate of area loss, however, increased over the period 2001–2006; −19.3 ± 2.4 km2 yr−1 (−2.0 ± 0.2% yr−1). Applying size class-specific scaling factors, we estimate a total reduction in glacier cover in the central and southern Canadian Rocky Mountains for the period 1919–2006 of 750 km2 (30%). Article in Journal/Newspaper The Cryosphere Unknown The Cryosphere 6 6 1541 1552 |
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envir geo C. Tennant B. Menounos R. Wheate J. J. Clague Area change of glaciers in the Canadian Rocky Mountains, 1919 to 2006 |
topic_facet |
envir geo |
description |
Glaciers in the Canadian Rocky Mountains constitute an important freshwater resource. To enhance our understanding of the influence climate and local topography have on glacier area, large numbers of glaciers of different sizes and attributes need to be monitored over periods of many decades. We used Interprovincial Boundary Commission Survey (IBCS) maps of the Alberta–British Columbia (BC) border (1903–1924), BC Terrain Resource Information Management (TRIM) data (1982–1987), and Landsat Thematic Mapper (TM) and Enhanced Thematic Mapper (ETM+) imagery (2000–2002 and 2006) to document planimetric changes in glacier cover in the central and southern Canadian Rocky Mountains between 1919 and 2006. Over this period, glacier cover in the study area decreased by 590 ± 70 km2 (40 ± 5%), 17 of 523 glaciers disappeared and 124 glaciers fragmented into multiple ice masses. Glaciers smaller than 1.0 km2 experienced the greatest relative area loss (64 ± 8%), and relative area loss is more variable with small glaciers, suggesting that the local topographic setting controls the response of these glaciers to climate change. Small glaciers with low slopes, low mean/median elevations, south to west aspects, and high insolation experienced the largest reduction in area. Similar rates of area change characterize the periods 1919–1985 and 1985–2001; −6.3 ± 0.6 km2 yr−1 (−0.4 ± 0.1% yr−1) and −5.0 ± 0.5 km2 yr−1 (−0.5 ± 0.1% yr−1), respectively. The rate of area loss, however, increased over the period 2001–2006; −19.3 ± 2.4 km2 yr−1 (−2.0 ± 0.2% yr−1). Applying size class-specific scaling factors, we estimate a total reduction in glacier cover in the central and southern Canadian Rocky Mountains for the period 1919–2006 of 750 km2 (30%). |
format |
Article in Journal/Newspaper |
author |
C. Tennant B. Menounos R. Wheate J. J. Clague |
author_facet |
C. Tennant B. Menounos R. Wheate J. J. Clague |
author_sort |
C. Tennant |
title |
Area change of glaciers in the Canadian Rocky Mountains, 1919 to 2006 |
title_short |
Area change of glaciers in the Canadian Rocky Mountains, 1919 to 2006 |
title_full |
Area change of glaciers in the Canadian Rocky Mountains, 1919 to 2006 |
title_fullStr |
Area change of glaciers in the Canadian Rocky Mountains, 1919 to 2006 |
title_full_unstemmed |
Area change of glaciers in the Canadian Rocky Mountains, 1919 to 2006 |
title_sort |
area change of glaciers in the canadian rocky mountains, 1919 to 2006 |
publisher |
Copernicus Publications |
publishDate |
2012 |
url |
https://doi.org/10.5194/tc-6-1541-2012 http://www.the-cryosphere.net/6/1541/2012/tc-6-1541-2012.pdf https://doaj.org/article/cf6671264f9d4c50bf591cc002952947 |
genre |
The Cryosphere |
genre_facet |
The Cryosphere |
op_source |
The Cryosphere, Vol 6, Iss 6, Pp 1541-1552 (2012) |
op_relation |
doi:10.5194/tc-6-1541-2012 1994-0416 1994-0424 http://www.the-cryosphere.net/6/1541/2012/tc-6-1541-2012.pdf https://doaj.org/article/cf6671264f9d4c50bf591cc002952947 |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/tc-6-1541-2012 |
container_title |
The Cryosphere |
container_volume |
6 |
container_issue |
6 |
container_start_page |
1541 |
op_container_end_page |
1552 |
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1766216465466261504 |