LAKE

LAKE is an extended one-dimensional model of thermodynamic, hydrodynamic and biogeochemical processes in the water basin and the bottom sediments (Stepanenko and Lykosov 2005, Stepanenko et al. 2011). The model simulates vertical heat transfer taking into account the penetration of short-wave radiat...

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Main Author: Victor, Stepanenko
Format: Article in Journal/Newspaper
Language:English
Published: Zenodo 2022
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.6353237
https://zenodo.org/record/6353237
id ftdatacite:10.5281/zenodo.6353237
record_format openpolar
spelling ftdatacite:10.5281/zenodo.6353237 2023-05-15T18:32:58+02:00 LAKE Victor, Stepanenko 2022 https://dx.doi.org/10.5281/zenodo.6353237 https://zenodo.org/record/6353237 en eng Zenodo https://dx.doi.org/10.5281/zenodo.6353238 Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess CC-BY lake thermodynamics hydrodynamics biogeochemistry mechanistic model greenhouse gases SoftwareSourceCode Software article 2022 ftdatacite https://doi.org/10.5281/zenodo.6353237 https://doi.org/10.5281/zenodo.6353238 2022-04-01T15:07:32Z LAKE is an extended one-dimensional model of thermodynamic, hydrodynamic and biogeochemical processes in the water basin and the bottom sediments (Stepanenko and Lykosov 2005, Stepanenko et al. 2011). The model simulates vertical heat transfer taking into account the penetration of short-wave radiation in water layers (Heiskanen et al., 2015), ice, snow and bottom sediments. The model allows for the evolution of ice layer at the bottom after complete lake freezing in winter. The equations of the model are formulated in terms of quantities averaged over the horizontal section a water body, which leads to an explicit account of the exchange of momentum, heat, and dissolved gases between water and the inclined bottom. In the water column, k−ϵ parametrization of turbulence is applied. The equations of motion take into account the barotropic (Stepanenko et al., 2016) and baroclinic pressure gradient (Степаненко, 2018). In ice and snow, a coupled transport of heat and liquid water is reproduced (Volodina et al. 2000; Stepanenko et al., 2019). In bottom sediments, water phase changes are simulated. The model also describes vertical diffusion of dissolved gases (CO2, CH4, O2), as well as their bubble transfer, methane oxidation, photosynthesis and processes of oxygen consumption. Parameterization of methane production in sediments is included (Stepanenko et al. 2011), and for the case of thermokarst lakes, an original formulation for the methane production near the lower boundary of "talik" is implemented. Model was tested in respect to thermal and ice regime at a number reservoirs in contrasting climate conditions, specifically, within the LakeMIP project (Lake Model Intercomparison Project, Stepanenko et al., 2010; Stepanenko et al., 2013; Stepanenko et al., 2014; Thiery et al., 2014). Article in Journal/Newspaper Thermokarst DataCite Metadata Store (German National Library of Science and Technology) Talik ENVELOPE(146.601,146.601,59.667,59.667)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic lake
thermodynamics
hydrodynamics
biogeochemistry
mechanistic model
greenhouse gases
spellingShingle lake
thermodynamics
hydrodynamics
biogeochemistry
mechanistic model
greenhouse gases
Victor, Stepanenko
LAKE
topic_facet lake
thermodynamics
hydrodynamics
biogeochemistry
mechanistic model
greenhouse gases
description LAKE is an extended one-dimensional model of thermodynamic, hydrodynamic and biogeochemical processes in the water basin and the bottom sediments (Stepanenko and Lykosov 2005, Stepanenko et al. 2011). The model simulates vertical heat transfer taking into account the penetration of short-wave radiation in water layers (Heiskanen et al., 2015), ice, snow and bottom sediments. The model allows for the evolution of ice layer at the bottom after complete lake freezing in winter. The equations of the model are formulated in terms of quantities averaged over the horizontal section a water body, which leads to an explicit account of the exchange of momentum, heat, and dissolved gases between water and the inclined bottom. In the water column, k−ϵ parametrization of turbulence is applied. The equations of motion take into account the barotropic (Stepanenko et al., 2016) and baroclinic pressure gradient (Степаненко, 2018). In ice and snow, a coupled transport of heat and liquid water is reproduced (Volodina et al. 2000; Stepanenko et al., 2019). In bottom sediments, water phase changes are simulated. The model also describes vertical diffusion of dissolved gases (CO2, CH4, O2), as well as their bubble transfer, methane oxidation, photosynthesis and processes of oxygen consumption. Parameterization of methane production in sediments is included (Stepanenko et al. 2011), and for the case of thermokarst lakes, an original formulation for the methane production near the lower boundary of "talik" is implemented. Model was tested in respect to thermal and ice regime at a number reservoirs in contrasting climate conditions, specifically, within the LakeMIP project (Lake Model Intercomparison Project, Stepanenko et al., 2010; Stepanenko et al., 2013; Stepanenko et al., 2014; Thiery et al., 2014).
format Article in Journal/Newspaper
author Victor, Stepanenko
author_facet Victor, Stepanenko
author_sort Victor, Stepanenko
title LAKE
title_short LAKE
title_full LAKE
title_fullStr LAKE
title_full_unstemmed LAKE
title_sort lake
publisher Zenodo
publishDate 2022
url https://dx.doi.org/10.5281/zenodo.6353237
https://zenodo.org/record/6353237
long_lat ENVELOPE(146.601,146.601,59.667,59.667)
geographic Talik
geographic_facet Talik
genre Thermokarst
genre_facet Thermokarst
op_relation https://dx.doi.org/10.5281/zenodo.6353238
op_rights Open Access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.5281/zenodo.6353237
https://doi.org/10.5281/zenodo.6353238
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