The influence of changes in glacier extent and surface elevation on modeled mass balance

Glaciers are widely recognized as unique demonstration objects for climate change impacts, mostly due to the strong change of glacier length in response to small climatic changes. However, glacier mass balance as the direct response to the annual atmospheric conditions can be better interpreted in m...

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Published in:The Cryosphere
Main Author: F. Paul
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2010
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-4-569-2010
http://www.the-cryosphere.net/4/569/2010/tc-4-569-2010.pdf
https://doaj.org/article/2b20dea430c2498cb3c426fd8952ecba
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:2b20dea430c2498cb3c426fd8952ecba 2023-05-15T18:32:23+02:00 The influence of changes in glacier extent and surface elevation on modeled mass balance F. Paul 2010-12-01 https://doi.org/10.5194/tc-4-569-2010 http://www.the-cryosphere.net/4/569/2010/tc-4-569-2010.pdf https://doaj.org/article/2b20dea430c2498cb3c426fd8952ecba en eng Copernicus Publications doi:10.5194/tc-4-569-2010 1994-0416 1994-0424 http://www.the-cryosphere.net/4/569/2010/tc-4-569-2010.pdf https://doaj.org/article/2b20dea430c2498cb3c426fd8952ecba undefined The Cryosphere, Vol 4, Iss 4, Pp 569-581 (2010) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2010 fttriple https://doi.org/10.5194/tc-4-569-2010 2023-01-22T19:30:59Z Glaciers are widely recognized as unique demonstration objects for climate change impacts, mostly due to the strong change of glacier length in response to small climatic changes. However, glacier mass balance as the direct response to the annual atmospheric conditions can be better interpreted in meteorological terms. When the climatic signal is deduced from long-term mass balance data, changes in glacier geometry (i.e. surface extent and elevation) must be considered as such adjustments form an essential part of the glacier reaction to new climatic conditions. In this study, a set of modelling experiments is performed to assess the influence of changes in glacier geometry on mass balance for constant climatic conditions. The calculations are based on a simplified distributed energy/mass balance model in combination with information on glacier extent and surface elevation for the years 1850 and 1973/1985 for about 60 glaciers in the Swiss Alps. The results reveal that over this period about 50–70% of the glacier reaction to climate change (here a one degree increase in temperature) is "hidden" in the geometric adjustment, while only 30–50% can be measured as the long-term mean mass balance. For larger glaciers, the effect of the areal change is partly reduced by a lowered surface elevation, which results in a slightly more negative balance despite a potential increase of topographic shading. In view of several additional reinforcement feedbacks that are observed in periods of strong glacier decline, it seems that the climatic interpretation of long-term mass balance data is rather complex. Article in Journal/Newspaper The Cryosphere Unknown The Cryosphere 4 4 569 581
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
F. Paul
The influence of changes in glacier extent and surface elevation on modeled mass balance
topic_facet geo
envir
description Glaciers are widely recognized as unique demonstration objects for climate change impacts, mostly due to the strong change of glacier length in response to small climatic changes. However, glacier mass balance as the direct response to the annual atmospheric conditions can be better interpreted in meteorological terms. When the climatic signal is deduced from long-term mass balance data, changes in glacier geometry (i.e. surface extent and elevation) must be considered as such adjustments form an essential part of the glacier reaction to new climatic conditions. In this study, a set of modelling experiments is performed to assess the influence of changes in glacier geometry on mass balance for constant climatic conditions. The calculations are based on a simplified distributed energy/mass balance model in combination with information on glacier extent and surface elevation for the years 1850 and 1973/1985 for about 60 glaciers in the Swiss Alps. The results reveal that over this period about 50–70% of the glacier reaction to climate change (here a one degree increase in temperature) is "hidden" in the geometric adjustment, while only 30–50% can be measured as the long-term mean mass balance. For larger glaciers, the effect of the areal change is partly reduced by a lowered surface elevation, which results in a slightly more negative balance despite a potential increase of topographic shading. In view of several additional reinforcement feedbacks that are observed in periods of strong glacier decline, it seems that the climatic interpretation of long-term mass balance data is rather complex.
format Article in Journal/Newspaper
author F. Paul
author_facet F. Paul
author_sort F. Paul
title The influence of changes in glacier extent and surface elevation on modeled mass balance
title_short The influence of changes in glacier extent and surface elevation on modeled mass balance
title_full The influence of changes in glacier extent and surface elevation on modeled mass balance
title_fullStr The influence of changes in glacier extent and surface elevation on modeled mass balance
title_full_unstemmed The influence of changes in glacier extent and surface elevation on modeled mass balance
title_sort influence of changes in glacier extent and surface elevation on modeled mass balance
publisher Copernicus Publications
publishDate 2010
url https://doi.org/10.5194/tc-4-569-2010
http://www.the-cryosphere.net/4/569/2010/tc-4-569-2010.pdf
https://doaj.org/article/2b20dea430c2498cb3c426fd8952ecba
genre The Cryosphere
genre_facet The Cryosphere
op_source The Cryosphere, Vol 4, Iss 4, Pp 569-581 (2010)
op_relation doi:10.5194/tc-4-569-2010
1994-0416
1994-0424
http://www.the-cryosphere.net/4/569/2010/tc-4-569-2010.pdf
https://doaj.org/article/2b20dea430c2498cb3c426fd8952ecba
op_rights undefined
op_doi https://doi.org/10.5194/tc-4-569-2010
container_title The Cryosphere
container_volume 4
container_issue 4
container_start_page 569
op_container_end_page 581
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