Variations in the Glacier Mass of Jostedalsbreen
Abstract By comparing the recorded run-off from a precipitation district, about 55 per cent of which is covered by glaciers, to the run-off from a neighbouring district without glaciers it has been possible to determine the changes in the glacier mass of Jostedalsbreen. In the period 1900 to 1940 th...
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Language: | English |
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Cambridge University Press (CUP)
1951
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Online Access: | http://dx.doi.org/10.1017/s0022143000026228 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000026228 |
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crcambridgeupr:10.1017/s0022143000026228 2024-10-20T14:09:52+00:00 Variations in the Glacier Mass of Jostedalsbreen Rogstad, Olaf 1951 http://dx.doi.org/10.1017/s0022143000026228 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000026228 en eng Cambridge University Press (CUP) Journal of Glaciology volume 1, issue 10, page 551-556 ISSN 0022-1430 1727-5652 journal-article 1951 crcambridgeupr https://doi.org/10.1017/s0022143000026228 2024-09-25T04:03:17Z Abstract By comparing the recorded run-off from a precipitation district, about 55 per cent of which is covered by glaciers, to the run-off from a neighbouring district without glaciers it has been possible to determine the changes in the glacier mass of Jostedalsbreen. In the period 1900 to 1940 the annual decrease of the glacier mass was equivalent to 0.4 m. of water times the glaciated area. A close relationship is established between the change of the glacier mass and the length of one of the outflow glaciers, Brikadalsbreen. It is shown that the change in the glacier mass is related to the summer temperature and, to a minor extent, to the amount of winter snowfall. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 1 10 551 556 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Abstract By comparing the recorded run-off from a precipitation district, about 55 per cent of which is covered by glaciers, to the run-off from a neighbouring district without glaciers it has been possible to determine the changes in the glacier mass of Jostedalsbreen. In the period 1900 to 1940 the annual decrease of the glacier mass was equivalent to 0.4 m. of water times the glaciated area. A close relationship is established between the change of the glacier mass and the length of one of the outflow glaciers, Brikadalsbreen. It is shown that the change in the glacier mass is related to the summer temperature and, to a minor extent, to the amount of winter snowfall. |
format |
Article in Journal/Newspaper |
author |
Rogstad, Olaf |
spellingShingle |
Rogstad, Olaf Variations in the Glacier Mass of Jostedalsbreen |
author_facet |
Rogstad, Olaf |
author_sort |
Rogstad, Olaf |
title |
Variations in the Glacier Mass of Jostedalsbreen |
title_short |
Variations in the Glacier Mass of Jostedalsbreen |
title_full |
Variations in the Glacier Mass of Jostedalsbreen |
title_fullStr |
Variations in the Glacier Mass of Jostedalsbreen |
title_full_unstemmed |
Variations in the Glacier Mass of Jostedalsbreen |
title_sort |
variations in the glacier mass of jostedalsbreen |
publisher |
Cambridge University Press (CUP) |
publishDate |
1951 |
url |
http://dx.doi.org/10.1017/s0022143000026228 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000026228 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 1, issue 10, page 551-556 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000026228 |
container_title |
Journal of Glaciology |
container_volume |
1 |
container_issue |
10 |
container_start_page |
551 |
op_container_end_page |
556 |
_version_ |
1813449524765523968 |