Ice Phenology and Thickness Modelling for Lake Ice Climatology

Analytic methods are useful for lake ice climatology investigations that account for ice phenology, thickness, and extent. Ice climatology depends on the local climate and lake characteristics, which can be compressed into a few forcing factors for analytic modelling. The internal factors are lake d...

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Main Author: Matti Leppäranta
Format: Article
Language:English
Published: MDPI AG 2023-08-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/15/16/2951
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author Matti Leppäranta
author_facet Matti Leppäranta
author_sort Matti Leppäranta
collection DOAJ
description Analytic methods are useful for lake ice climatology investigations that account for ice phenology, thickness, and extent. Ice climatology depends on the local climate and lake characteristics, which can be compressed into a few forcing factors for analytic modelling. The internal factors are lake depth, size, and water quality, while the external factors are solar radiation, air–lake interaction, and heat flux from bottom sediment. A two-layer temperature structure with a sharp thermocline in-between is employed for the water body and a non-inert conduction law for the ice cover. A thermal equilibrium approach results in temperature and ice thickness solutions, and a time scale analysis provides the applicability of the equilibrium method for lake ice climatology. A non-steady solution is needed for ice melting.
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spelling doaj.art-f0e904dd166444f5a02cd675554f1e472023-11-19T03:23:07ZengMDPI AGWater2073-44412023-08-011516295110.3390/w15162951Ice Phenology and Thickness Modelling for Lake Ice ClimatologyMatti Leppäranta0Institute of Atmospheric and Earth Sciences, University of Helsinki, 00014 Helsinki, FinlandAnalytic methods are useful for lake ice climatology investigations that account for ice phenology, thickness, and extent. Ice climatology depends on the local climate and lake characteristics, which can be compressed into a few forcing factors for analytic modelling. The internal factors are lake depth, size, and water quality, while the external factors are solar radiation, air–lake interaction, and heat flux from bottom sediment. A two-layer temperature structure with a sharp thermocline in-between is employed for the water body and a non-inert conduction law for the ice cover. A thermal equilibrium approach results in temperature and ice thickness solutions, and a time scale analysis provides the applicability of the equilibrium method for lake ice climatology. A non-steady solution is needed for ice melting.https://www.mdpi.com/2073-4441/15/16/2951lake iceclimatologyphenologymodellingequilibrium
spellingShingle Matti Leppäranta
Ice Phenology and Thickness Modelling for Lake Ice Climatology
Water
lake ice
climatology
phenology
modelling
equilibrium
title Ice Phenology and Thickness Modelling for Lake Ice Climatology
title_full Ice Phenology and Thickness Modelling for Lake Ice Climatology
title_fullStr Ice Phenology and Thickness Modelling for Lake Ice Climatology
title_full_unstemmed Ice Phenology and Thickness Modelling for Lake Ice Climatology
title_short Ice Phenology and Thickness Modelling for Lake Ice Climatology
title_sort ice phenology and thickness modelling for lake ice climatology
topic lake ice
climatology
phenology
modelling
equilibrium
url https://www.mdpi.com/2073-4441/15/16/2951
work_keys_str_mv AT mattilepparanta icephenologyandthicknessmodellingforlakeiceclimatology