Simulation of temperate freezing lakes by one-dimensional lake models : performance assessment for interactive coupling with regional climate models

A systematic assessment of the ability of two selected 1-D lake models (the model of S.W. Hostetler and the Freshwater Lake model) to simulate lake surface temperature and fluxes for different lake conditions, corresponding to typical temperate freezing lakes of North America, through a set of offline tests, is presented.Results suggest that both models perform well in shallow lakes, while important differences between modelled and observed water temperatures and ice-cover duration can be noticed in deeper lakes.These differences could be partially attributed to the biases in the driving data and most importantly to the lack of representation of complex processes in the models, such as horizontal transfer of water and heat, ice drift, etc. Sensitivity of the models to lake depth, water transparency, explicit snow and snow/ice albedo is presented and possible ways of improving the performance of the 1-D lake models are proposed.

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Publication Details

Journal
Työväentutkimus Vuosikirja
Published
2024-12-12
DOI
https://doi.org/10.60910/4emh-6f4w
Citations
114
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
Field-Weighted Citation Impact
3.01

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article

Simulation of temperate freezing lakes by one-dimensional lake models : performance assessment for interactive coupling with regional climate models

Laxmi Sushama, Andrey Martynov, René Laprise
114 citations
Työväentutkimus Vuosikirja
Arctic and Antarctic ice dynamics
3.01
article

Simulation of temperate freezing lakes by one-dimensional lake models : performance assessment for interactive coupling with regional climate models

Laxmi Sushama, Andrey Martynov, René Laprise
article en
114 citations

Abstract

A systematic assessment of the ability of two selected 1-D lake models (the model of S.W. Hostetler and the Freshwater Lake model) to simulate lake surface temperature and fluxes for different lake conditions, corresponding to typical temperate freezing lakes of North America, through a set of offline tests, is presented.Results suggest that both models perform well in shallow lakes, while important differences between modelled and observed water temperatures and ice-cover duration can be noticed in deeper lakes.These differences could be partially attributed to the biases in the driving data and most importantly to the lack of representation of complex processes in the models, such as horizontal transfer of water and heat, ice drift, etc. Sensitivity of the models to lake depth, water transparency, explicit snow and snow/ice albedo is presented and possible ways of improving the performance of the 1-D lake models are proposed.

Työväentutkimus VuosikirjaVol. 15(2)
National Science Foundation, University of Wisconsin-Madison, Canadian Foundation for Climate and Atmospheric Sciences
Climate action
Openalex Percentile: Top 10%
Arctic and Antarctic ice dynamics
3.01
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