Application of a simple model for ice growth to the Lake St. Moritz, Switzerland

We present a Simple Lake Ice Model to calculate the growth rate of lake ice in a cold and relatively dry climate. The focus is on Lake St. Moritz, Switzerland, which has an area of 0.78 km² and is about 45 m deep. In winter the lake is extensively used for recreational purposes, including horse raci...

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Main Authors: Oerlemans, Johannes, Keller, Felix
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2023
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/626974
https://doi.org/10.3929/ethz-b-000626974
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spelling ftethz:oai:www.research-collection.ethz.ch:20.500.11850/626974 2023-09-05T13:20:43+02:00 Application of a simple model for ice growth to the Lake St. Moritz, Switzerland Oerlemans, Johannes Keller, Felix 2023-08 application/application/pdf https://hdl.handle.net/20.500.11850/626974 https://doi.org/10.3929/ethz-b-000626974 en eng Cambridge University Press info:eu-repo/semantics/altIdentifier/doi/10.1017/jog.2022.110 info:eu-repo/semantics/altIdentifier/wos/001038121200032 http://hdl.handle.net/20.500.11850/626974 doi:10.3929/ethz-b-000626974 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International Journal of Glaciology, 69 (276) Ice/atmosphere interactions lake ice snow/ice surface processes info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2023 ftethz https://doi.org/20.500.11850/62697410.3929/ethz-b-00062697410.1017/jog.2022.110 2023-08-20T23:49:23Z We present a Simple Lake Ice Model to calculate the growth rate of lake ice in a cold and relatively dry climate. The focus is on Lake St. Moritz, Switzerland, which has an area of 0.78 km² and is about 45 m deep. In winter the lake is extensively used for recreational purposes, including horse racing with thousands of spectators. Safety on the ice cover is essential, and there is a great need to have a simple tool with which the growth rate of the ice layer can be calculated for given meteorological conditions. The approach is based on a simple formulation of the upper temperature of the ice layer, which depends on air temperature and snow cover. Input data are the date on which the lake freezes over, daily mean air temperatures and snow depth. For the winter 2021/22 calculated ice growth compares well with ice thickness measurements. We demonstrate that grooming of the snow has a significant positive effect on the ice thickening rate. We also evaluate the sensitivity of the simulated ice thickness to increasing mean temperature. ISSN:0022-1430 ISSN:1727-5652 Article in Journal/Newspaper Journal of Glaciology ETH Zürich Research Collection
institution Open Polar
collection ETH Zürich Research Collection
op_collection_id ftethz
language English
topic Ice/atmosphere interactions
lake ice
snow/ice surface processes
spellingShingle Ice/atmosphere interactions
lake ice
snow/ice surface processes
Oerlemans, Johannes
Keller, Felix
Application of a simple model for ice growth to the Lake St. Moritz, Switzerland
topic_facet Ice/atmosphere interactions
lake ice
snow/ice surface processes
description We present a Simple Lake Ice Model to calculate the growth rate of lake ice in a cold and relatively dry climate. The focus is on Lake St. Moritz, Switzerland, which has an area of 0.78 km² and is about 45 m deep. In winter the lake is extensively used for recreational purposes, including horse racing with thousands of spectators. Safety on the ice cover is essential, and there is a great need to have a simple tool with which the growth rate of the ice layer can be calculated for given meteorological conditions. The approach is based on a simple formulation of the upper temperature of the ice layer, which depends on air temperature and snow cover. Input data are the date on which the lake freezes over, daily mean air temperatures and snow depth. For the winter 2021/22 calculated ice growth compares well with ice thickness measurements. We demonstrate that grooming of the snow has a significant positive effect on the ice thickening rate. We also evaluate the sensitivity of the simulated ice thickness to increasing mean temperature. ISSN:0022-1430 ISSN:1727-5652
format Article in Journal/Newspaper
author Oerlemans, Johannes
Keller, Felix
author_facet Oerlemans, Johannes
Keller, Felix
author_sort Oerlemans, Johannes
title Application of a simple model for ice growth to the Lake St. Moritz, Switzerland
title_short Application of a simple model for ice growth to the Lake St. Moritz, Switzerland
title_full Application of a simple model for ice growth to the Lake St. Moritz, Switzerland
title_fullStr Application of a simple model for ice growth to the Lake St. Moritz, Switzerland
title_full_unstemmed Application of a simple model for ice growth to the Lake St. Moritz, Switzerland
title_sort application of a simple model for ice growth to the lake st. moritz, switzerland
publisher Cambridge University Press
publishDate 2023
url https://hdl.handle.net/20.500.11850/626974
https://doi.org/10.3929/ethz-b-000626974
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology, 69 (276)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1017/jog.2022.110
info:eu-repo/semantics/altIdentifier/wos/001038121200032
http://hdl.handle.net/20.500.11850/626974
doi:10.3929/ethz-b-000626974
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International
op_doi https://doi.org/20.500.11850/62697410.3929/ethz-b-00062697410.1017/jog.2022.110
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