Landsat-derived glacier inventory for Jotunheimen, Norway, and deduced glacier changes since the 1930s

A Landsat Thematic Mapper (TM) scene from 2003 covering the Jotunheimen and Breheimen region has been used to map the recent glacier extents using thresholded ratio images (TM3/TM5). Orthoprojected aerial photographs and glacier outlines from digital maps have been used to validate the method and co...

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Main Authors: L. M. Andreassen, F. Paul, A. Kääb, J. E. Hausberg
Format: Article
Language:English
Published: Copernicus Publications 2008-10-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/2/131/2008/tc-2-131-2008.pdf
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spelling doaj-d077fd6db0d84fbfa452bbda20f2d74d2020-11-25T00:29:45ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242008-10-0122131145Landsat-derived glacier inventory for Jotunheimen, Norway, and deduced glacier changes since the 1930sL. M. AndreassenF. PaulA. KääbJ. E. HausbergA Landsat Thematic Mapper (TM) scene from 2003 covering the Jotunheimen and Breheimen region has been used to map the recent glacier extents using thresholded ratio images (TM3/TM5). Orthoprojected aerial photographs and glacier outlines from digital maps have been used to validate the method and control the results. We further calculated glacier changes by comparing the Landsat-derived 2003 glacier outlines with previous maps and inventories from the 1930s, 1960s and 1980s. Our results confirm that the applied automatic mapping method is robust and agrees with the reference data used. Some manual editing was necessary to correct the outline at ice-lake contacts and at debris covered glaciers. However, for most of the glaciers no corrections were required. The most laborious task has been to assign ID numbers and couple the new Landsat inventory to previous inventories to assess area changes. The glaciers investigated shrank since the 1930s with an overall area reduction of about 23% for 38 glaciers. Since the 1960s the area reduction was 12% for 164 glaciers. Although the general trend is glacier recession, some glaciers have increased their size or remained nearly unchanged over these decades. http://www.the-cryosphere.net/2/131/2008/tc-2-131-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author L. M. Andreassen
F. Paul
A. Kääb
J. E. Hausberg
spellingShingle L. M. Andreassen
F. Paul
A. Kääb
J. E. Hausberg
Landsat-derived glacier inventory for Jotunheimen, Norway, and deduced glacier changes since the 1930s
The Cryosphere
author_facet L. M. Andreassen
F. Paul
A. Kääb
J. E. Hausberg
author_sort L. M. Andreassen
title Landsat-derived glacier inventory for Jotunheimen, Norway, and deduced glacier changes since the 1930s
title_short Landsat-derived glacier inventory for Jotunheimen, Norway, and deduced glacier changes since the 1930s
title_full Landsat-derived glacier inventory for Jotunheimen, Norway, and deduced glacier changes since the 1930s
title_fullStr Landsat-derived glacier inventory for Jotunheimen, Norway, and deduced glacier changes since the 1930s
title_full_unstemmed Landsat-derived glacier inventory for Jotunheimen, Norway, and deduced glacier changes since the 1930s
title_sort landsat-derived glacier inventory for jotunheimen, norway, and deduced glacier changes since the 1930s
publisher Copernicus Publications
series The Cryosphere
issn 1994-0416
1994-0424
publishDate 2008-10-01
description A Landsat Thematic Mapper (TM) scene from 2003 covering the Jotunheimen and Breheimen region has been used to map the recent glacier extents using thresholded ratio images (TM3/TM5). Orthoprojected aerial photographs and glacier outlines from digital maps have been used to validate the method and control the results. We further calculated glacier changes by comparing the Landsat-derived 2003 glacier outlines with previous maps and inventories from the 1930s, 1960s and 1980s. Our results confirm that the applied automatic mapping method is robust and agrees with the reference data used. Some manual editing was necessary to correct the outline at ice-lake contacts and at debris covered glaciers. However, for most of the glaciers no corrections were required. The most laborious task has been to assign ID numbers and couple the new Landsat inventory to previous inventories to assess area changes. The glaciers investigated shrank since the 1930s with an overall area reduction of about 23% for 38 glaciers. Since the 1960s the area reduction was 12% for 164 glaciers. Although the general trend is glacier recession, some glaciers have increased their size or remained nearly unchanged over these decades.
url http://www.the-cryosphere.net/2/131/2008/tc-2-131-2008.pdf
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