Subglacial Water Pressures and the Shape of Subglacial Conduits

Abstract Measured subglacial water pressures are frequently higher than theoretical values calculated by assuming that subglacial conduits are straight and either circular or semi-circular in shape. While this may be attributed to errors in the estimates of conduit roughness or ice viscosity, we sug...

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Published in:Journal of Glaciology
Main Authors: Hooke, Roger LeB., Laumann, Tron, Kohler, Jack
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1990
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000005566
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000005566
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spelling crcambridgeupr:10.1017/s0022143000005566 2023-06-11T04:13:26+02:00 Subglacial Water Pressures and the Shape of Subglacial Conduits Hooke, Roger LeB. Laumann, Tron Kohler, Jack 1990 http://dx.doi.org/10.1017/s0022143000005566 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000005566 en eng Cambridge University Press (CUP) Journal of Glaciology volume 36, issue 122, page 67-71 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1990 crcambridgeupr https://doi.org/10.1017/s0022143000005566 2023-05-01T18:21:50Z Abstract Measured subglacial water pressures are frequently higher than theoretical values calculated by assuming that subglacial conduits are straight and either circular or semi-circular in shape. While this may be attributed to errors in the estimates of conduit roughness or ice viscosity, we suggest here an alternative explanation: namely, that the conduits are actually broad and low rather than semi-circular. Good agreement between measured and calculated pressures can be obtained by assuming that the cross-sectional shape of conduits resembles the space between the arc of a circle and its chord. The angle subtended by the arc, θ, is treated as an adjustable parameter. In four cases studied, θ ranged from 2° to 36°. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press (via Crossref) Journal of Glaciology 36 122 67 71
institution Open Polar
collection Cambridge University Press (via Crossref)
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Hooke, Roger LeB.
Laumann, Tron
Kohler, Jack
Subglacial Water Pressures and the Shape of Subglacial Conduits
topic_facet Earth-Surface Processes
description Abstract Measured subglacial water pressures are frequently higher than theoretical values calculated by assuming that subglacial conduits are straight and either circular or semi-circular in shape. While this may be attributed to errors in the estimates of conduit roughness or ice viscosity, we suggest here an alternative explanation: namely, that the conduits are actually broad and low rather than semi-circular. Good agreement between measured and calculated pressures can be obtained by assuming that the cross-sectional shape of conduits resembles the space between the arc of a circle and its chord. The angle subtended by the arc, θ, is treated as an adjustable parameter. In four cases studied, θ ranged from 2° to 36°.
format Article in Journal/Newspaper
author Hooke, Roger LeB.
Laumann, Tron
Kohler, Jack
author_facet Hooke, Roger LeB.
Laumann, Tron
Kohler, Jack
author_sort Hooke, Roger LeB.
title Subglacial Water Pressures and the Shape of Subglacial Conduits
title_short Subglacial Water Pressures and the Shape of Subglacial Conduits
title_full Subglacial Water Pressures and the Shape of Subglacial Conduits
title_fullStr Subglacial Water Pressures and the Shape of Subglacial Conduits
title_full_unstemmed Subglacial Water Pressures and the Shape of Subglacial Conduits
title_sort subglacial water pressures and the shape of subglacial conduits
publisher Cambridge University Press (CUP)
publishDate 1990
url http://dx.doi.org/10.1017/s0022143000005566
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000005566
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 36, issue 122, page 67-71
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000005566
container_title Journal of Glaciology
container_volume 36
container_issue 122
container_start_page 67
op_container_end_page 71
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