Glacier change in northern Sweden from AD 500: a simple geometric model of Storglaciären
Abstract A simple geometric model of glacier volume is derived. The model is based on the assumption that the net mass balance averaged over the glacier surface is related to the summer temperature and winter accumulation at a representative height on the glacier. This height varies with time as cli...
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Language: | English |
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Cambridge University Press (CUP)
1996
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Online Access: | http://dx.doi.org/10.1017/s0022143000004196 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000004196 |
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crcambridgeupr:10.1017/s0022143000004196 2024-03-03T08:44:17+00:00 Glacier change in northern Sweden from AD 500: a simple geometric model of Storglaciären Raper, S. C. В. Briffa, K. R. Wigley, Т. M. L. 1996 http://dx.doi.org/10.1017/s0022143000004196 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000004196 en eng Cambridge University Press (CUP) Journal of Glaciology volume 42, issue 141, page 341-351 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1996 crcambridgeupr https://doi.org/10.1017/s0022143000004196 2024-02-08T08:36:10Z Abstract A simple geometric model of glacier volume is derived. The model is based on the assumption that the net mass balance averaged over the glacier surface is related to the summer temperature and winter accumulation at a representative height on the glacier. This height varies with time as climate changes, in ways that are determined by the geometry of the glacier surface. Expressions are derived for the equilibrium glacier volume ( V eq ) as a function of summer temperature and winter accumulation and for the glacier-response time ( τ ) as a function of volume. The model is used to reconstruct the volume of Storglaciären over the period AD 500–1992. Measured net mass-balance data for Storglaciren (1946–92) are used to estimate the model parameters. For the summer temperature forcing, the long tree-ring-based temperature reconstruction for northern Fennoscandia is used to extend a temperature record near the glacier back to AD 500. For the past accumulation forcing, a range of assumptions is tested. The results show that the prime cause of the decrease in volume of Storglaciären between 1946 and 1992 was relatively low accumulation over 1946–89 as opposed to warm temperatures as previously supposed. Reconstructed volume changes agree well with geomorphological evidence. Where differences occur, deductions can be made about past accumulation. For example, the maximum reconstructed glacier volume is associated with the cold period from 1580 to 1740 but relatively low accumulation probably limited the volume to values not much larger than that achieved around 1916. Article in Journal/Newspaper Fennoscandia Journal of Glaciology Northern Sweden Cambridge University Press Storglaciären ENVELOPE(18.560,18.560,67.904,67.904) Journal of Glaciology 42 141 341 351 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Raper, S. C. В. Briffa, K. R. Wigley, Т. M. L. Glacier change in northern Sweden from AD 500: a simple geometric model of Storglaciären |
topic_facet |
Earth-Surface Processes |
description |
Abstract A simple geometric model of glacier volume is derived. The model is based on the assumption that the net mass balance averaged over the glacier surface is related to the summer temperature and winter accumulation at a representative height on the glacier. This height varies with time as climate changes, in ways that are determined by the geometry of the glacier surface. Expressions are derived for the equilibrium glacier volume ( V eq ) as a function of summer temperature and winter accumulation and for the glacier-response time ( τ ) as a function of volume. The model is used to reconstruct the volume of Storglaciären over the period AD 500–1992. Measured net mass-balance data for Storglaciren (1946–92) are used to estimate the model parameters. For the summer temperature forcing, the long tree-ring-based temperature reconstruction for northern Fennoscandia is used to extend a temperature record near the glacier back to AD 500. For the past accumulation forcing, a range of assumptions is tested. The results show that the prime cause of the decrease in volume of Storglaciären between 1946 and 1992 was relatively low accumulation over 1946–89 as opposed to warm temperatures as previously supposed. Reconstructed volume changes agree well with geomorphological evidence. Where differences occur, deductions can be made about past accumulation. For example, the maximum reconstructed glacier volume is associated with the cold period from 1580 to 1740 but relatively low accumulation probably limited the volume to values not much larger than that achieved around 1916. |
format |
Article in Journal/Newspaper |
author |
Raper, S. C. В. Briffa, K. R. Wigley, Т. M. L. |
author_facet |
Raper, S. C. В. Briffa, K. R. Wigley, Т. M. L. |
author_sort |
Raper, S. C. В. |
title |
Glacier change in northern Sweden from AD 500: a simple geometric model of Storglaciären |
title_short |
Glacier change in northern Sweden from AD 500: a simple geometric model of Storglaciären |
title_full |
Glacier change in northern Sweden from AD 500: a simple geometric model of Storglaciären |
title_fullStr |
Glacier change in northern Sweden from AD 500: a simple geometric model of Storglaciären |
title_full_unstemmed |
Glacier change in northern Sweden from AD 500: a simple geometric model of Storglaciären |
title_sort |
glacier change in northern sweden from ad 500: a simple geometric model of storglaciären |
publisher |
Cambridge University Press (CUP) |
publishDate |
1996 |
url |
http://dx.doi.org/10.1017/s0022143000004196 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000004196 |
long_lat |
ENVELOPE(18.560,18.560,67.904,67.904) |
geographic |
Storglaciären |
geographic_facet |
Storglaciären |
genre |
Fennoscandia Journal of Glaciology Northern Sweden |
genre_facet |
Fennoscandia Journal of Glaciology Northern Sweden |
op_source |
Journal of Glaciology volume 42, issue 141, page 341-351 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000004196 |
container_title |
Journal of Glaciology |
container_volume |
42 |
container_issue |
141 |
container_start_page |
341 |
op_container_end_page |
351 |
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1792499776422412288 |