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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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Johannes Oerlemans, Felix Keller
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2023
Subjects:
Online Access:https://doi.org/10.1017/jog.2022.110
https://doaj.org/article/5536b0256c6b43e2928ff36858229a30
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spelling ftdoajarticles:oai:doaj.org/article:5536b0256c6b43e2928ff36858229a30 2023-08-20T04:07:38+02:00 Application of a simple model for ice growth to the Lake St. Moritz, Switzerland Johannes Oerlemans Felix Keller 2023-08-01T00:00:00Z https://doi.org/10.1017/jog.2022.110 https://doaj.org/article/5536b0256c6b43e2928ff36858229a30 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022001101/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.110 0022-1430 1727-5652 https://doaj.org/article/5536b0256c6b43e2928ff36858229a30 Journal of Glaciology, Vol 69, Pp 1085-1090 (2023) Ice/atmosphere interactions lake ice snow/ice surface processes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1017/jog.2022.110 2023-07-30T00:36:44Z 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. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 1 6
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Ice/atmosphere interactions
lake ice
snow/ice surface processes
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Ice/atmosphere interactions
lake ice
snow/ice surface processes
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Johannes Oerlemans
Felix Keller
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
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
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.
format Article in Journal/Newspaper
author Johannes Oerlemans
Felix Keller
author_facet Johannes Oerlemans
Felix Keller
author_sort Johannes Oerlemans
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://doi.org/10.1017/jog.2022.110
https://doaj.org/article/5536b0256c6b43e2928ff36858229a30
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology, Vol 69, Pp 1085-1090 (2023)
op_relation https://www.cambridge.org/core/product/identifier/S0022143022001101/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2022.110
0022-1430
1727-5652
https://doaj.org/article/5536b0256c6b43e2928ff36858229a30
op_doi https://doi.org/10.1017/jog.2022.110
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 6
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