Sensitivity of Rhonegletscher, Switzerland, to climate change : Experiments with a one-dimensional flowline model

A one-dimensional time-dependent flowline model of Rhonegletscher, Switzerland, has been used to test the glacier's response to climatic warming. Mass-balance variations over the last 100 years are obtained from observations of the equilibrium-line altitude (ELA) and a reconstruction of the ELA...

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Published in:Journal of Glaciology
Main Author: Wallinga, Jakob
Format: Article in Journal/Newspaper
Language:English
Published: 1998
Subjects:
Ela
Online Access:https://research.wur.nl/en/publications/sensitivity-of-rhonegletscher-switzerland-to-climate-change-exper
https://doi.org/10.1017/S0022143000002719
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spelling ftunivwagenin:oai:library.wur.nl:wurpubs/562331 2024-02-04T10:01:42+01:00 Sensitivity of Rhonegletscher, Switzerland, to climate change : Experiments with a one-dimensional flowline model Wallinga, Jakob 1998 text/html https://research.wur.nl/en/publications/sensitivity-of-rhonegletscher-switzerland-to-climate-change-exper https://doi.org/10.1017/S0022143000002719 en eng https://edepot.wur.nl/517635 https://research.wur.nl/en/publications/sensitivity-of-rhonegletscher-switzerland-to-climate-change-exper doi:10.1017/S0022143000002719 info:eu-repo/semantics/restrictedAccess Wageningen University & Research Journal of Glaciology 44 (1998) 147 ISSN: 0022-1430 Life Science info:eu-repo/semantics/article Article/Letter to editor info:eu-repo/semantics/publishedVersion 1998 ftunivwagenin https://doi.org/10.1017/S0022143000002719 2024-01-10T23:28:44Z A one-dimensional time-dependent flowline model of Rhonegletscher, Switzerland, has been used to test the glacier's response to climatic warming. Mass-balance variations over the last 100 years are obtained from observations of the equilibrium-line altitude (ELA) and a reconstruction of the ELA based on a statistical correlation between temperature and ELA. For the period prior to AD 1882, for which no reliable climate data exist, we chose equilibrium-line altitudes that enabled us to simulate accurately the glacier length from AD 1602. The model simulates the historical glacier length almost perfectly and glacier geometry very well. It underestimates glacier-surface velocities by 1-18%. Following these reference experiments, we investigated the response of Rhonegletscher to a number of climate-change scenarios for the period AD 1990-2100. For a constant climate equal to the 1961-90 mean, the model predicts a 6% decrease in glacier volume by AD 2100. Rhonegletscher will retreat by almost 1 km over the next 100 years at this scenario. At a warming rate of 0.04 K a-1, only 4% of the glacier volume will be left by AD 2100. Article in Journal/Newspaper Journal of Glaciology Wageningen UR (University & Research Centre): Digital Library Ela ENVELOPE(9.642,9.642,63.170,63.170) Journal of Glaciology 44 147 383 393
institution Open Polar
collection Wageningen UR (University & Research Centre): Digital Library
op_collection_id ftunivwagenin
language English
topic Life Science
spellingShingle Life Science
Wallinga, Jakob
Sensitivity of Rhonegletscher, Switzerland, to climate change : Experiments with a one-dimensional flowline model
topic_facet Life Science
description A one-dimensional time-dependent flowline model of Rhonegletscher, Switzerland, has been used to test the glacier's response to climatic warming. Mass-balance variations over the last 100 years are obtained from observations of the equilibrium-line altitude (ELA) and a reconstruction of the ELA based on a statistical correlation between temperature and ELA. For the period prior to AD 1882, for which no reliable climate data exist, we chose equilibrium-line altitudes that enabled us to simulate accurately the glacier length from AD 1602. The model simulates the historical glacier length almost perfectly and glacier geometry very well. It underestimates glacier-surface velocities by 1-18%. Following these reference experiments, we investigated the response of Rhonegletscher to a number of climate-change scenarios for the period AD 1990-2100. For a constant climate equal to the 1961-90 mean, the model predicts a 6% decrease in glacier volume by AD 2100. Rhonegletscher will retreat by almost 1 km over the next 100 years at this scenario. At a warming rate of 0.04 K a-1, only 4% of the glacier volume will be left by AD 2100.
format Article in Journal/Newspaper
author Wallinga, Jakob
author_facet Wallinga, Jakob
author_sort Wallinga, Jakob
title Sensitivity of Rhonegletscher, Switzerland, to climate change : Experiments with a one-dimensional flowline model
title_short Sensitivity of Rhonegletscher, Switzerland, to climate change : Experiments with a one-dimensional flowline model
title_full Sensitivity of Rhonegletscher, Switzerland, to climate change : Experiments with a one-dimensional flowline model
title_fullStr Sensitivity of Rhonegletscher, Switzerland, to climate change : Experiments with a one-dimensional flowline model
title_full_unstemmed Sensitivity of Rhonegletscher, Switzerland, to climate change : Experiments with a one-dimensional flowline model
title_sort sensitivity of rhonegletscher, switzerland, to climate change : experiments with a one-dimensional flowline model
publishDate 1998
url https://research.wur.nl/en/publications/sensitivity-of-rhonegletscher-switzerland-to-climate-change-exper
https://doi.org/10.1017/S0022143000002719
long_lat ENVELOPE(9.642,9.642,63.170,63.170)
geographic Ela
geographic_facet Ela
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology 44 (1998) 147
ISSN: 0022-1430
op_relation https://edepot.wur.nl/517635
https://research.wur.nl/en/publications/sensitivity-of-rhonegletscher-switzerland-to-climate-change-exper
doi:10.1017/S0022143000002719
op_rights info:eu-repo/semantics/restrictedAccess
Wageningen University & Research
op_doi https://doi.org/10.1017/S0022143000002719
container_title Journal of Glaciology
container_volume 44
container_issue 147
container_start_page 383
op_container_end_page 393
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