The Magnitude of Jökulhlaups
A review of available information on six self-dumping glacier-dammed lakes indicates that instantaneous discharge during a jökulhlaup is proportional to some power of the cumulative volume of water released rather than being a direct function of time. Information on these and four other self-dumping...
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Language: | English |
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Cambridge University Press (CUP)
1973
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Online Access: | http://dx.doi.org/10.1017/s0022143000031907 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031907 |
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crcambridgeupr:10.1017/s0022143000031907 2024-09-15T18:15:39+00:00 The Magnitude of Jökulhlaups Clague, J. J. Mathews, W. H. 1973 http://dx.doi.org/10.1017/s0022143000031907 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031907 en eng Cambridge University Press (CUP) Journal of Glaciology volume 12, issue 66, page 501-504 ISSN 0022-1430 1727-5652 journal-article 1973 crcambridgeupr https://doi.org/10.1017/s0022143000031907 2024-07-31T04:03:51Z A review of available information on six self-dumping glacier-dammed lakes indicates that instantaneous discharge during a jökulhlaup is proportional to some power of the cumulative volume of water released rather than being a direct function of time. Information on these and four other self-dumping lakes, moreover, indicates that the peak discharge at the end of each jökulhlaup is approximately proportional to the two-thirds power of the total volume of water released during the flood. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 12 66 501 504 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
A review of available information on six self-dumping glacier-dammed lakes indicates that instantaneous discharge during a jökulhlaup is proportional to some power of the cumulative volume of water released rather than being a direct function of time. Information on these and four other self-dumping lakes, moreover, indicates that the peak discharge at the end of each jökulhlaup is approximately proportional to the two-thirds power of the total volume of water released during the flood. |
format |
Article in Journal/Newspaper |
author |
Clague, J. J. Mathews, W. H. |
spellingShingle |
Clague, J. J. Mathews, W. H. The Magnitude of Jökulhlaups |
author_facet |
Clague, J. J. Mathews, W. H. |
author_sort |
Clague, J. J. |
title |
The Magnitude of Jökulhlaups |
title_short |
The Magnitude of Jökulhlaups |
title_full |
The Magnitude of Jökulhlaups |
title_fullStr |
The Magnitude of Jökulhlaups |
title_full_unstemmed |
The Magnitude of Jökulhlaups |
title_sort |
magnitude of jökulhlaups |
publisher |
Cambridge University Press (CUP) |
publishDate |
1973 |
url |
http://dx.doi.org/10.1017/s0022143000031907 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031907 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 12, issue 66, page 501-504 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000031907 |
container_title |
Journal of Glaciology |
container_volume |
12 |
container_issue |
66 |
container_start_page |
501 |
op_container_end_page |
504 |
_version_ |
1810453570961539072 |