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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Published in:Journal of Glaciology
Main Author: Rogstad, Olaf
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1951
Subjects:
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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spelling 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
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