High-resolution measurements of spatial and temporal variations in surface velocities of Unteraargletscher, Bernese Alps, Switzerland

Data from automated in situ measurements of surface displacements on Unteraargletscher, Bernese Alps, Switzerland, made a few times a day from late June until late October 1998 are presented. Two short-term speed-up events were observed, and partial evidence for a third motion event was seen. Short-...

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Published in:Annals of Glaciology
Main Authors: Gudmundsson, Hilmar, Bassi, A., Vonmoos, M., Bauder, Andreas, Fischer, U. H., Funk, Martin
Format: Article in Journal/Newspaper
Language:unknown
Published: International Glaciological Society 2000
Subjects:
Online Access:https://nrl.northumbria.ac.uk/id/eprint/38035/
https://doi.org/10.3189/172756400781820156
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author Gudmundsson, Hilmar
Bassi, A.
Vonmoos, M.
Bauder, Andreas
Fischer, U. H.
Funk, Martin
author_facet Gudmundsson, Hilmar
Bassi, A.
Vonmoos, M.
Bauder, Andreas
Fischer, U. H.
Funk, Martin
author_sort Gudmundsson, Hilmar
collection Northumbria University, Newcastle: Northumbria Research Link (NRL)
container_start_page 63
container_title Annals of Glaciology
container_volume 31
description Data from automated in situ measurements of surface displacements on Unteraargletscher, Bernese Alps, Switzerland, made a few times a day from late June until late October 1998 are presented. Two short-term speed-up events were observed, and partial evidence for a third motion event was seen. Short-term motion events are thus not limited to the start of the melting season. Strong correlation between the timing of the motion events and periods of heavy rainfall, in conjunction with the large size of the area of the glacier which becomes activated during the events, both point towards an external triggering mechanism. In the time periods between two motion events, surface velocities do not vary significantly with time. After a motion event, surface velocities do not return to previous values, suggesting that the events have a lasting effect on the structure of the subglacial drainage system.
format Article in Journal/Newspaper
genre Annals of Glaciology
genre_facet Annals of Glaciology
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institution Open Polar
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op_container_end_page 68
op_doi https://doi.org/10.3189/172756400781820156
op_relation Gudmundsson, Hilmar, Bassi, A., Vonmoos, M., Bauder, Andreas, Fischer, U. H. and Funk, Martin (2000) High-resolution measurements of spatial and temporal variations in surface velocities of Unteraargletscher, Bernese Alps, Switzerland. Annals of Glaciology, 31. pp. 63-68. ISSN 0260-3055
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spelling ftunivnorthumb:oai:nrl.northumbria.ac.uk:38035 2025-01-16T19:00:05+00:00 High-resolution measurements of spatial and temporal variations in surface velocities of Unteraargletscher, Bernese Alps, Switzerland Gudmundsson, Hilmar Bassi, A. Vonmoos, M. Bauder, Andreas Fischer, U. H. Funk, Martin 2000 https://nrl.northumbria.ac.uk/id/eprint/38035/ https://doi.org/10.3189/172756400781820156 unknown International Glaciological Society Gudmundsson, Hilmar, Bassi, A., Vonmoos, M., Bauder, Andreas, Fischer, U. H. and Funk, Martin (2000) High-resolution measurements of spatial and temporal variations in surface velocities of Unteraargletscher, Bernese Alps, Switzerland. Annals of Glaciology, 31. pp. 63-68. ISSN 0260-3055 F800 Physical and Terrestrial Geographical and Environmental Sciences Article PeerReviewed 2000 ftunivnorthumb https://doi.org/10.3189/172756400781820156 2022-09-25T06:09:12Z Data from automated in situ measurements of surface displacements on Unteraargletscher, Bernese Alps, Switzerland, made a few times a day from late June until late October 1998 are presented. Two short-term speed-up events were observed, and partial evidence for a third motion event was seen. Short-term motion events are thus not limited to the start of the melting season. Strong correlation between the timing of the motion events and periods of heavy rainfall, in conjunction with the large size of the area of the glacier which becomes activated during the events, both point towards an external triggering mechanism. In the time periods between two motion events, surface velocities do not vary significantly with time. After a motion event, surface velocities do not return to previous values, suggesting that the events have a lasting effect on the structure of the subglacial drainage system. Article in Journal/Newspaper Annals of Glaciology Northumbria University, Newcastle: Northumbria Research Link (NRL) Annals of Glaciology 31 63 68
spellingShingle F800 Physical and Terrestrial Geographical and Environmental Sciences
Gudmundsson, Hilmar
Bassi, A.
Vonmoos, M.
Bauder, Andreas
Fischer, U. H.
Funk, Martin
High-resolution measurements of spatial and temporal variations in surface velocities of Unteraargletscher, Bernese Alps, Switzerland
title High-resolution measurements of spatial and temporal variations in surface velocities of Unteraargletscher, Bernese Alps, Switzerland
title_full High-resolution measurements of spatial and temporal variations in surface velocities of Unteraargletscher, Bernese Alps, Switzerland
title_fullStr High-resolution measurements of spatial and temporal variations in surface velocities of Unteraargletscher, Bernese Alps, Switzerland
title_full_unstemmed High-resolution measurements of spatial and temporal variations in surface velocities of Unteraargletscher, Bernese Alps, Switzerland
title_short High-resolution measurements of spatial and temporal variations in surface velocities of Unteraargletscher, Bernese Alps, Switzerland
title_sort high-resolution measurements of spatial and temporal variations in surface velocities of unteraargletscher, bernese alps, switzerland
topic F800 Physical and Terrestrial Geographical and Environmental Sciences
topic_facet F800 Physical and Terrestrial Geographical and Environmental Sciences
url https://nrl.northumbria.ac.uk/id/eprint/38035/
https://doi.org/10.3189/172756400781820156