Brief communication: Growth and decay of an ice stupa in alpine conditions - a simple model driven by energy-flux observations over a glacier surface

We present a simple model to calculate the evolution of an ice stupa (artificial ice reservoir). The model is formulated for a cone geometry and driven by energy balance measurements over a glacier surface for a 5-year period. An "exposure factor"is introduced to deal with the fact that an...

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Main Authors: Oerlemans, Johannes, Balasubramanian, Suryanarayanan, Clavuot, Conradin, Keller, Felix
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus 2021
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/493464
https://doi.org/10.3929/ethz-b-000493464
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spelling ftethz:oai:www.research-collection.ethz.ch:20.500.11850/493464 2023-05-15T18:32:14+02:00 Brief communication: Growth and decay of an ice stupa in alpine conditions - a simple model driven by energy-flux observations over a glacier surface Oerlemans, Johannes Balasubramanian, Suryanarayanan Clavuot, Conradin Keller, Felix 2021-06-29 application/application/pdf https://hdl.handle.net/20.500.11850/493464 https://doi.org/10.3929/ethz-b-000493464 en eng Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-15-3007-2021 info:eu-repo/semantics/altIdentifier/wos/000669514200002 http://hdl.handle.net/20.500.11850/493464 doi:10.3929/ethz-b-000493464 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International CC-BY The Cryosphere, 15 (6) info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2021 ftethz https://doi.org/20.500.11850/493464 https://doi.org/10.3929/ethz-b-000493464 https://doi.org/10.5194/tc-15-3007-2021 2022-04-25T14:31:30Z We present a simple model to calculate the evolution of an ice stupa (artificial ice reservoir). The model is formulated for a cone geometry and driven by energy balance measurements over a glacier surface for a 5-year period. An "exposure factor"is introduced to deal with the fact that an ice stupa has a very rough surface and is more exposed to wind than a flat glacier surface. The exposure factor enhances the turbulent fluxes. For characteristic alpine conditions at 2100gm, an ice stupa may reach a volume of 200 to 400gm3 in early April. We show sensitivities of ice stupa size to temperature changes and exposure factor. The model may also serve as an educational tool, with which the effects of snow cover, switching off water during daytime, different starting dates, switching off water during high wind speeds, etc. can easily be evaluated. ISSN:1994-0416 ISSN:1994-0424 Article in Journal/Newspaper The Cryosphere ETH Zürich Research Collection Stupa ENVELOPE(22.166,22.166,70.636,70.636)
institution Open Polar
collection ETH Zürich Research Collection
op_collection_id ftethz
language English
description We present a simple model to calculate the evolution of an ice stupa (artificial ice reservoir). The model is formulated for a cone geometry and driven by energy balance measurements over a glacier surface for a 5-year period. An "exposure factor"is introduced to deal with the fact that an ice stupa has a very rough surface and is more exposed to wind than a flat glacier surface. The exposure factor enhances the turbulent fluxes. For characteristic alpine conditions at 2100gm, an ice stupa may reach a volume of 200 to 400gm3 in early April. We show sensitivities of ice stupa size to temperature changes and exposure factor. The model may also serve as an educational tool, with which the effects of snow cover, switching off water during daytime, different starting dates, switching off water during high wind speeds, etc. can easily be evaluated. ISSN:1994-0416 ISSN:1994-0424
format Article in Journal/Newspaper
author Oerlemans, Johannes
Balasubramanian, Suryanarayanan
Clavuot, Conradin
Keller, Felix
spellingShingle Oerlemans, Johannes
Balasubramanian, Suryanarayanan
Clavuot, Conradin
Keller, Felix
Brief communication: Growth and decay of an ice stupa in alpine conditions - a simple model driven by energy-flux observations over a glacier surface
author_facet Oerlemans, Johannes
Balasubramanian, Suryanarayanan
Clavuot, Conradin
Keller, Felix
author_sort Oerlemans, Johannes
title Brief communication: Growth and decay of an ice stupa in alpine conditions - a simple model driven by energy-flux observations over a glacier surface
title_short Brief communication: Growth and decay of an ice stupa in alpine conditions - a simple model driven by energy-flux observations over a glacier surface
title_full Brief communication: Growth and decay of an ice stupa in alpine conditions - a simple model driven by energy-flux observations over a glacier surface
title_fullStr Brief communication: Growth and decay of an ice stupa in alpine conditions - a simple model driven by energy-flux observations over a glacier surface
title_full_unstemmed Brief communication: Growth and decay of an ice stupa in alpine conditions - a simple model driven by energy-flux observations over a glacier surface
title_sort brief communication: growth and decay of an ice stupa in alpine conditions - a simple model driven by energy-flux observations over a glacier surface
publisher Copernicus
publishDate 2021
url https://hdl.handle.net/20.500.11850/493464
https://doi.org/10.3929/ethz-b-000493464
long_lat ENVELOPE(22.166,22.166,70.636,70.636)
geographic Stupa
geographic_facet Stupa
genre The Cryosphere
genre_facet The Cryosphere
op_source The Cryosphere, 15 (6)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-15-3007-2021
info:eu-repo/semantics/altIdentifier/wos/000669514200002
http://hdl.handle.net/20.500.11850/493464
doi:10.3929/ethz-b-000493464
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International
op_rightsnorm CC-BY
op_doi https://doi.org/20.500.11850/493464
https://doi.org/10.3929/ethz-b-000493464
https://doi.org/10.5194/tc-15-3007-2021
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