Width and length scaling of glaciers
Abstract An analysis of hundreds of mountain and valley glaciers in the former Soviet Union and the Alps shows that characteristic glacier widths scale as characteristic glacier lengths raised to an exponent of 0.6. This is in contrast to most previous analyses which implicitly of explicitly assumed...
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Language: | English |
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Cambridge University Press (CUP)
1997
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Online Access: | http://dx.doi.org/10.1017/s0022143000035164 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000035164 |
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crcambridgeupr:10.1017/s0022143000035164 2024-09-15T18:15:39+00:00 Width and length scaling of glaciers Bahr, David B. 1997 http://dx.doi.org/10.1017/s0022143000035164 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000035164 en eng Cambridge University Press (CUP) Journal of Glaciology volume 43, issue 145, page 557-562 ISSN 0022-1430 1727-5652 journal-article 1997 crcambridgeupr https://doi.org/10.1017/s0022143000035164 2024-06-26T04:03:41Z Abstract An analysis of hundreds of mountain and valley glaciers in the former Soviet Union and the Alps shows that characteristic glacier widths scale as characteristic glacier lengths raised to an exponent of 0.6. This is in contrast to most previous analyses which implicitly of explicitly assumed scaling exponents of either 0 or 1. The exponent 0.6 implies that average glacier widths are proportional to average glacier thicknesses. Although this seems to suggest V-shaped glacier valleys, the linear width-thickness relationship is not inconsistent with parabolic valley cross-sections, because the characteristic (or average) width of a glacier depends on many other aspects of channel and glacier morphology, including variations in the channel width with distance up- and downstream. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 43 145 557 562 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Abstract An analysis of hundreds of mountain and valley glaciers in the former Soviet Union and the Alps shows that characteristic glacier widths scale as characteristic glacier lengths raised to an exponent of 0.6. This is in contrast to most previous analyses which implicitly of explicitly assumed scaling exponents of either 0 or 1. The exponent 0.6 implies that average glacier widths are proportional to average glacier thicknesses. Although this seems to suggest V-shaped glacier valleys, the linear width-thickness relationship is not inconsistent with parabolic valley cross-sections, because the characteristic (or average) width of a glacier depends on many other aspects of channel and glacier morphology, including variations in the channel width with distance up- and downstream. |
format |
Article in Journal/Newspaper |
author |
Bahr, David B. |
spellingShingle |
Bahr, David B. Width and length scaling of glaciers |
author_facet |
Bahr, David B. |
author_sort |
Bahr, David B. |
title |
Width and length scaling of glaciers |
title_short |
Width and length scaling of glaciers |
title_full |
Width and length scaling of glaciers |
title_fullStr |
Width and length scaling of glaciers |
title_full_unstemmed |
Width and length scaling of glaciers |
title_sort |
width and length scaling of glaciers |
publisher |
Cambridge University Press (CUP) |
publishDate |
1997 |
url |
http://dx.doi.org/10.1017/s0022143000035164 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000035164 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 43, issue 145, page 557-562 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000035164 |
container_title |
Journal of Glaciology |
container_volume |
43 |
container_issue |
145 |
container_start_page |
557 |
op_container_end_page |
562 |
_version_ |
1810453539565076480 |