Short-term velocity and water-pressure variations down-glacier from a riegel, Storglaciären, Sweden
Abstract During the 1991 94 summer held seasons, time-correlated measure-merits of water pressure and surface speed were made over and down-glacier from a major riegel on Storglaciären, Sweden. Measurements were made at sub-hourly time-scales in order to discern details in the diurnal cycle. Large w...
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1998
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Online Access: | http://dx.doi.org/10.1017/s0022143000002689 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000002689 |
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crcambridgeupr:10.1017/s0022143000002689 2024-03-03T08:46:08+00:00 Short-term velocity and water-pressure variations down-glacier from a riegel, Storglaciären, Sweden Hanson, Brian LeB. Hooke, Roger Grace, Edmund M. 1998 http://dx.doi.org/10.1017/s0022143000002689 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000002689 en eng Cambridge University Press (CUP) Journal of Glaciology volume 44, issue 147, page 359-367 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1998 crcambridgeupr https://doi.org/10.1017/s0022143000002689 2024-02-08T08:41:37Z Abstract During the 1991 94 summer held seasons, time-correlated measure-merits of water pressure and surface speed were made over and down-glacier from a major riegel on Storglaciären, Sweden. Measurements were made at sub-hourly time-scales in order to discern details in the diurnal cycle. Large water-input events, typically associated with rain storms, produced coherent, lagged surface-velocity responses that could be understood in terms of till deformation or decoupling, and these have been discussed elsewhere. The consequences of smaller diurnal water-pressure events w ere more enigmatic, in that acceleration of ice flow generally preceded the onset of the local water-pressure rise. From consideration of these data and other work done on the hydrology of Storglaciären, we infer that the ice in this area is generally pushed from behind via a relaxation in extensional strain across the riegel. Hence, accelerations occur in response to increases in water pressure that occur up-glacier and that precede local water-pressure rises. In addition, following a period of large storm events, surface speeds became more spatially coherent and were in phase with the diurnal water-pressure cycle. This suggests that the large water-pressure events lead to a spatially more homogeneous subglacial drainage system. Sliding laws need to take into account such temporal changes in spatial coherence of the subglacial drainage system. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Storglaciären ENVELOPE(18.560,18.560,67.904,67.904) Journal of Glaciology 44 147 359 367 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Hanson, Brian LeB. Hooke, Roger Grace, Edmund M. Short-term velocity and water-pressure variations down-glacier from a riegel, Storglaciären, Sweden |
topic_facet |
Earth-Surface Processes |
description |
Abstract During the 1991 94 summer held seasons, time-correlated measure-merits of water pressure and surface speed were made over and down-glacier from a major riegel on Storglaciären, Sweden. Measurements were made at sub-hourly time-scales in order to discern details in the diurnal cycle. Large water-input events, typically associated with rain storms, produced coherent, lagged surface-velocity responses that could be understood in terms of till deformation or decoupling, and these have been discussed elsewhere. The consequences of smaller diurnal water-pressure events w ere more enigmatic, in that acceleration of ice flow generally preceded the onset of the local water-pressure rise. From consideration of these data and other work done on the hydrology of Storglaciären, we infer that the ice in this area is generally pushed from behind via a relaxation in extensional strain across the riegel. Hence, accelerations occur in response to increases in water pressure that occur up-glacier and that precede local water-pressure rises. In addition, following a period of large storm events, surface speeds became more spatially coherent and were in phase with the diurnal water-pressure cycle. This suggests that the large water-pressure events lead to a spatially more homogeneous subglacial drainage system. Sliding laws need to take into account such temporal changes in spatial coherence of the subglacial drainage system. |
format |
Article in Journal/Newspaper |
author |
Hanson, Brian LeB. Hooke, Roger Grace, Edmund M. |
author_facet |
Hanson, Brian LeB. Hooke, Roger Grace, Edmund M. |
author_sort |
Hanson, Brian |
title |
Short-term velocity and water-pressure variations down-glacier from a riegel, Storglaciären, Sweden |
title_short |
Short-term velocity and water-pressure variations down-glacier from a riegel, Storglaciären, Sweden |
title_full |
Short-term velocity and water-pressure variations down-glacier from a riegel, Storglaciären, Sweden |
title_fullStr |
Short-term velocity and water-pressure variations down-glacier from a riegel, Storglaciären, Sweden |
title_full_unstemmed |
Short-term velocity and water-pressure variations down-glacier from a riegel, Storglaciären, Sweden |
title_sort |
short-term velocity and water-pressure variations down-glacier from a riegel, storglaciären, sweden |
publisher |
Cambridge University Press (CUP) |
publishDate |
1998 |
url |
http://dx.doi.org/10.1017/s0022143000002689 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000002689 |
long_lat |
ENVELOPE(18.560,18.560,67.904,67.904) |
geographic |
Storglaciären |
geographic_facet |
Storglaciären |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 44, issue 147, page 359-367 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000002689 |
container_title |
Journal of Glaciology |
container_volume |
44 |
container_issue |
147 |
container_start_page |
359 |
op_container_end_page |
367 |
_version_ |
1792502066391810048 |