Glacier fluctuations of Jostedalsbreen, western Norway, during the past 20 years: the sensitive response of maritime mountain glaciers

The steep outlet glaciers of Jostedalsbreen, western Norway, are good examples of sensitively reacting maritime mountain glaciers. Their changes in length, frontal position and lower tongue's morphology during the past 20 years have been well documented. At first they experienced a strong front...

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Published in:The Holocene
Main Authors: Winkler, Stefan, Elvehøy, Hallgeir, Nesje, Atle
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 2009
Subjects:
Online Access:http://dx.doi.org/10.1177/0959683608101390
http://journals.sagepub.com/doi/pdf/10.1177/0959683608101390
id crsagepubl:10.1177/0959683608101390
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spelling crsagepubl:10.1177/0959683608101390 2024-09-15T18:07:51+00:00 Glacier fluctuations of Jostedalsbreen, western Norway, during the past 20 years: the sensitive response of maritime mountain glaciers Winkler, Stefan Elvehøy, Hallgeir Nesje, Atle 2009 http://dx.doi.org/10.1177/0959683608101390 http://journals.sagepub.com/doi/pdf/10.1177/0959683608101390 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license The Holocene volume 19, issue 3, page 395-414 ISSN 0959-6836 1477-0911 journal-article 2009 crsagepubl https://doi.org/10.1177/0959683608101390 2024-08-19T04:29:09Z The steep outlet glaciers of Jostedalsbreen, western Norway, are good examples of sensitively reacting maritime mountain glaciers. Their changes in length, frontal position and lower tongue's morphology during the past 20 years have been well documented. At first they experienced a strong frontal advance. After AD 2000 glacier behaviour was dominated by a strong frontal retreat, in some cases causing a separation of the lowermost glacier tongue. In this paper, the glacier length changes are presented both visually and numerically, supplemented by mass balance and meteorological data. The glacier behaviour is interpreted and its causes are discussed. Whereas the factors controlling the advance during the 1990s seem clear, the interpretation of the most recent retreat still leaves some uncertainties. The actual glacier front behaviour cannot fully be related to the mass balance data. Terminus response times and relations between individual mass balance and meteorological parameters have changed. Some hypotheses are given, including disturbance of the `normal' mass transfer and dynamical response of the glacier front because of excessive ablation on the lowermost glacier tongues and summer back melting. These findings underline the sensitivity of maritime glaciers to climate changes. The empirical findings need to be taken into account in the interpretation of recent glacier length changes and their future modelling. Article in Journal/Newspaper glacier SAGE Publications The Holocene 19 3 395 414
institution Open Polar
collection SAGE Publications
op_collection_id crsagepubl
language English
description The steep outlet glaciers of Jostedalsbreen, western Norway, are good examples of sensitively reacting maritime mountain glaciers. Their changes in length, frontal position and lower tongue's morphology during the past 20 years have been well documented. At first they experienced a strong frontal advance. After AD 2000 glacier behaviour was dominated by a strong frontal retreat, in some cases causing a separation of the lowermost glacier tongue. In this paper, the glacier length changes are presented both visually and numerically, supplemented by mass balance and meteorological data. The glacier behaviour is interpreted and its causes are discussed. Whereas the factors controlling the advance during the 1990s seem clear, the interpretation of the most recent retreat still leaves some uncertainties. The actual glacier front behaviour cannot fully be related to the mass balance data. Terminus response times and relations between individual mass balance and meteorological parameters have changed. Some hypotheses are given, including disturbance of the `normal' mass transfer and dynamical response of the glacier front because of excessive ablation on the lowermost glacier tongues and summer back melting. These findings underline the sensitivity of maritime glaciers to climate changes. The empirical findings need to be taken into account in the interpretation of recent glacier length changes and their future modelling.
format Article in Journal/Newspaper
author Winkler, Stefan
Elvehøy, Hallgeir
Nesje, Atle
spellingShingle Winkler, Stefan
Elvehøy, Hallgeir
Nesje, Atle
Glacier fluctuations of Jostedalsbreen, western Norway, during the past 20 years: the sensitive response of maritime mountain glaciers
author_facet Winkler, Stefan
Elvehøy, Hallgeir
Nesje, Atle
author_sort Winkler, Stefan
title Glacier fluctuations of Jostedalsbreen, western Norway, during the past 20 years: the sensitive response of maritime mountain glaciers
title_short Glacier fluctuations of Jostedalsbreen, western Norway, during the past 20 years: the sensitive response of maritime mountain glaciers
title_full Glacier fluctuations of Jostedalsbreen, western Norway, during the past 20 years: the sensitive response of maritime mountain glaciers
title_fullStr Glacier fluctuations of Jostedalsbreen, western Norway, during the past 20 years: the sensitive response of maritime mountain glaciers
title_full_unstemmed Glacier fluctuations of Jostedalsbreen, western Norway, during the past 20 years: the sensitive response of maritime mountain glaciers
title_sort glacier fluctuations of jostedalsbreen, western norway, during the past 20 years: the sensitive response of maritime mountain glaciers
publisher SAGE Publications
publishDate 2009
url http://dx.doi.org/10.1177/0959683608101390
http://journals.sagepub.com/doi/pdf/10.1177/0959683608101390
genre glacier
genre_facet glacier
op_source The Holocene
volume 19, issue 3, page 395-414
ISSN 0959-6836 1477-0911
op_rights http://journals.sagepub.com/page/policies/text-and-data-mining-license
op_doi https://doi.org/10.1177/0959683608101390
container_title The Holocene
container_volume 19
container_issue 3
container_start_page 395
op_container_end_page 414
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