Decay of a High Arctic lake-ice cover: observations and modelling

Abstract The decay of a lake-ice cover in the Canadian High Arctic was studied for 2 years. Melt at the upper surface accounted for 75% of the decrease in ice thickness, while 25% occurred at the ice–water interface. An energy-balance model, incorporating density reduction due to internal ice melt,...

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Published in:Journal of Glaciology
Main Authors: Heron, Richard, Woo, Ming-Ko
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1994
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000007371
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000007371
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spelling crcambridgeupr:10.1017/s0022143000007371 2024-09-15T18:15:39+00:00 Decay of a High Arctic lake-ice cover: observations and modelling Heron, Richard Woo, Ming-Ko 1994 http://dx.doi.org/10.1017/s0022143000007371 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000007371 en eng Cambridge University Press (CUP) Journal of Glaciology volume 40, issue 135, page 283-292 ISSN 0022-1430 1727-5652 journal-article 1994 crcambridgeupr https://doi.org/10.1017/s0022143000007371 2024-07-10T04:02:33Z Abstract The decay of a lake-ice cover in the Canadian High Arctic was studied for 2 years. Melt at the upper surface accounted for 75% of the decrease in ice thickness, while 25% occurred at the ice–water interface. An energy-balance model, incorporating density reduction due to internal ice melt, was used to simulate the decay of the ice cover. The overall performance of the model was satisfactory despite periods when computed results differed from the observed ice decay. Energy-balance calculations indicated that the absorption of shortwave radiation within the ice provided 52% of the melt energy while 33 and 15% came from the surface-energy balance and heat flux from the water. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 40 135 283 292
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract The decay of a lake-ice cover in the Canadian High Arctic was studied for 2 years. Melt at the upper surface accounted for 75% of the decrease in ice thickness, while 25% occurred at the ice–water interface. An energy-balance model, incorporating density reduction due to internal ice melt, was used to simulate the decay of the ice cover. The overall performance of the model was satisfactory despite periods when computed results differed from the observed ice decay. Energy-balance calculations indicated that the absorption of shortwave radiation within the ice provided 52% of the melt energy while 33 and 15% came from the surface-energy balance and heat flux from the water.
format Article in Journal/Newspaper
author Heron, Richard
Woo, Ming-Ko
spellingShingle Heron, Richard
Woo, Ming-Ko
Decay of a High Arctic lake-ice cover: observations and modelling
author_facet Heron, Richard
Woo, Ming-Ko
author_sort Heron, Richard
title Decay of a High Arctic lake-ice cover: observations and modelling
title_short Decay of a High Arctic lake-ice cover: observations and modelling
title_full Decay of a High Arctic lake-ice cover: observations and modelling
title_fullStr Decay of a High Arctic lake-ice cover: observations and modelling
title_full_unstemmed Decay of a High Arctic lake-ice cover: observations and modelling
title_sort decay of a high arctic lake-ice cover: observations and modelling
publisher Cambridge University Press (CUP)
publishDate 1994
url http://dx.doi.org/10.1017/s0022143000007371
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000007371
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 40, issue 135, page 283-292
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000007371
container_title Journal of Glaciology
container_volume 40
container_issue 135
container_start_page 283
op_container_end_page 292
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