Short term variations of tracer transit speed on alpine glaciers

We first present the results of a series of tracer experiments conducted on an alpine glacier (Gornergletscher, Switzerland) over a diurnal discharge cycle. For these injections, a moulin was used into which an ice marginal lake was draining, providing a relatively constant discharge. The measured t...

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Published in:The Cryosphere
Main Authors: M. A. Werder, T. V. Schuler, M. Funk
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2010
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-4-381-2010
http://www.the-cryosphere.net/4/381/2010/tc-4-381-2010.pdf
https://doaj.org/article/7cd60b07ec0f4a2584b9e9cdeb04eec5
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:7cd60b07ec0f4a2584b9e9cdeb04eec5 2023-05-15T18:32:22+02:00 Short term variations of tracer transit speed on alpine glaciers M. A. Werder T. V. Schuler M. Funk 2010-09-01 https://doi.org/10.5194/tc-4-381-2010 http://www.the-cryosphere.net/4/381/2010/tc-4-381-2010.pdf https://doaj.org/article/7cd60b07ec0f4a2584b9e9cdeb04eec5 en eng Copernicus Publications doi:10.5194/tc-4-381-2010 1994-0416 1994-0424 http://www.the-cryosphere.net/4/381/2010/tc-4-381-2010.pdf https://doaj.org/article/7cd60b07ec0f4a2584b9e9cdeb04eec5 undefined The Cryosphere, Vol 4, Iss 3, Pp 381-396 (2010) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2010 fttriple https://doi.org/10.5194/tc-4-381-2010 2023-01-22T17:44:18Z We first present the results of a series of tracer experiments conducted on an alpine glacier (Gornergletscher, Switzerland) over a diurnal discharge cycle. For these injections, a moulin was used into which an ice marginal lake was draining, providing a relatively constant discharge. The measured tracer transit speeds show two diurnal maxima and minima. These findings are qualitatively different to existing observations from two series of injections conducted at Unteraargletscher (Switzerland) using a moulin fed by supraglacial meltwater having a high diurnal variability, which displayed one diurnal maximum and minimum. We then develop and use a simple two-component model of the glacier drainage system, comprising a moulin and a channel element, to simulate the measured transit speeds for all three injection series. The model successfully reproduces all the observations and shows that the same underlying processes can produce the qualitatively different behaviour depending on the different moulin input discharge regimes. Using the model, we assess the relative importance of the different measurement quantities, show that frequent measurements of moulin input discharge are indispensable and propose an experiment design to monitor the development of the drainage system over several weeks. Article in Journal/Newspaper The Cryosphere Unknown Marginal Lake ENVELOPE(163.500,163.500,-74.600,-74.600) The Cryosphere 4 3 381 396
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
M. A. Werder
T. V. Schuler
M. Funk
Short term variations of tracer transit speed on alpine glaciers
topic_facet geo
envir
description We first present the results of a series of tracer experiments conducted on an alpine glacier (Gornergletscher, Switzerland) over a diurnal discharge cycle. For these injections, a moulin was used into which an ice marginal lake was draining, providing a relatively constant discharge. The measured tracer transit speeds show two diurnal maxima and minima. These findings are qualitatively different to existing observations from two series of injections conducted at Unteraargletscher (Switzerland) using a moulin fed by supraglacial meltwater having a high diurnal variability, which displayed one diurnal maximum and minimum. We then develop and use a simple two-component model of the glacier drainage system, comprising a moulin and a channel element, to simulate the measured transit speeds for all three injection series. The model successfully reproduces all the observations and shows that the same underlying processes can produce the qualitatively different behaviour depending on the different moulin input discharge regimes. Using the model, we assess the relative importance of the different measurement quantities, show that frequent measurements of moulin input discharge are indispensable and propose an experiment design to monitor the development of the drainage system over several weeks.
format Article in Journal/Newspaper
author M. A. Werder
T. V. Schuler
M. Funk
author_facet M. A. Werder
T. V. Schuler
M. Funk
author_sort M. A. Werder
title Short term variations of tracer transit speed on alpine glaciers
title_short Short term variations of tracer transit speed on alpine glaciers
title_full Short term variations of tracer transit speed on alpine glaciers
title_fullStr Short term variations of tracer transit speed on alpine glaciers
title_full_unstemmed Short term variations of tracer transit speed on alpine glaciers
title_sort short term variations of tracer transit speed on alpine glaciers
publisher Copernicus Publications
publishDate 2010
url https://doi.org/10.5194/tc-4-381-2010
http://www.the-cryosphere.net/4/381/2010/tc-4-381-2010.pdf
https://doaj.org/article/7cd60b07ec0f4a2584b9e9cdeb04eec5
long_lat ENVELOPE(163.500,163.500,-74.600,-74.600)
geographic Marginal Lake
geographic_facet Marginal Lake
genre The Cryosphere
genre_facet The Cryosphere
op_source The Cryosphere, Vol 4, Iss 3, Pp 381-396 (2010)
op_relation doi:10.5194/tc-4-381-2010
1994-0416
1994-0424
http://www.the-cryosphere.net/4/381/2010/tc-4-381-2010.pdf
https://doaj.org/article/7cd60b07ec0f4a2584b9e9cdeb04eec5
op_rights undefined
op_doi https://doi.org/10.5194/tc-4-381-2010
container_title The Cryosphere
container_volume 4
container_issue 3
container_start_page 381
op_container_end_page 396
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