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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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Clague, J. J., Mathews, W. H.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1973
Subjects:
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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spelling 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
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