A 3D numerical modeling of the links between hydrodynamics, dissolved oxygen, and water temperature of a northern rural-urban shallow lake with two distinct basins
A 3D hydrodynamic model (EFDC) was applied to simulate dissolved oxygen (DO) and temperature (T) (two crucial parameters impacting water quality) throughout Lake St. Charles, a rural-urban shallow lake located North of Quebec City, Canada. Model outputs of T and DO corroborate observations at five m...
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Veröffentlicht in: | Environmental monitoring and assessment 2023-10, Vol.195 (10), p.1198-1198, Article 1198 |
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description | A 3D hydrodynamic model (EFDC) was applied to simulate dissolved oxygen (DO) and temperature (T) (two crucial parameters impacting water quality) throughout Lake St. Charles, a rural-urban shallow lake located North of Quebec City, Canada. Model outputs of T and DO corroborate observations at five monitoring stations within the lake. Simulated results indicated annual cycles of turnovers and stratifications and different behaviors for the deep and shallow basins. For the simulated years, the deep basin was stratified in summer and winter, while the shallow basin was mostly mixed throughout the year. The lake heat budget indicates that during summer with a long retention time, the thermal structure of the lake is principally controlled by net radiation, latent, and sensible heat fluxes. For the rest of the year, the inflow (from the main tributary, the Des Hurons River) and outflow are the main drivers of the lake’s thermal structure. |
doi_str_mv | 10.1007/s10661-023-11744-2 |
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Model outputs of T and DO corroborate observations at five monitoring stations within the lake. Simulated results indicated annual cycles of turnovers and stratifications and different behaviors for the deep and shallow basins. For the simulated years, the deep basin was stratified in summer and winter, while the shallow basin was mostly mixed throughout the year. The lake heat budget indicates that during summer with a long retention time, the thermal structure of the lake is principally controlled by net radiation, latent, and sensible heat fluxes. For the rest of the year, the inflow (from the main tributary, the Des Hurons River) and outflow are the main drivers of the lake’s thermal structure.</description><identifier>ISSN: 0167-6369</identifier><identifier>EISSN: 1573-2959</identifier><identifier>DOI: 10.1007/s10661-023-11744-2</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Algae ; Annual cycles ; Annual variations ; Aquatic ecosystems ; Aquatic life ; Atmospheric Protection/Air Quality Control/Air Pollution ; Basins ; Cyanobacteria ; Dissolved oxygen ; Drinking water ; Earth and Environmental Science ; Ecology ; Ecotoxicology ; Enthalpy ; Environment ; Environmental Management ; Environmental monitoring ; Fluid mechanics ; Heat budget ; Heat flux ; Heat transfer ; Hydrodynamic models ; Hydrodynamics ; Inflow ; Lakes ; Monitoring systems ; Monitoring/Environmental Analysis ; Net radiation ; Numerical models ; Outflow ; Oxygen ; Radiation balance ; Retention time ; Sensible heat ; Simulation ; Summer ; Thermal structure ; Three dimensional models ; Tributaries ; Water inflow ; Water outflow ; Water quality ; Water temperature ; Water treatment</subject><ispartof>Environmental monitoring and assessment, 2023-10, Vol.195 (10), p.1198-1198, Article 1198</ispartof><rights>The Author(s), under exclusive licence to Springer Nature Switzerland AG 2023. 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Model outputs of T and DO corroborate observations at five monitoring stations within the lake. Simulated results indicated annual cycles of turnovers and stratifications and different behaviors for the deep and shallow basins. For the simulated years, the deep basin was stratified in summer and winter, while the shallow basin was mostly mixed throughout the year. The lake heat budget indicates that during summer with a long retention time, the thermal structure of the lake is principally controlled by net radiation, latent, and sensible heat fluxes. For the rest of the year, the inflow (from the main tributary, the Des Hurons River) and outflow are the main drivers of the lake’s thermal structure.</description><subject>Algae</subject><subject>Annual cycles</subject><subject>Annual variations</subject><subject>Aquatic ecosystems</subject><subject>Aquatic life</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Basins</subject><subject>Cyanobacteria</subject><subject>Dissolved oxygen</subject><subject>Drinking water</subject><subject>Earth and Environmental Science</subject><subject>Ecology</subject><subject>Ecotoxicology</subject><subject>Enthalpy</subject><subject>Environment</subject><subject>Environmental Management</subject><subject>Environmental monitoring</subject><subject>Fluid mechanics</subject><subject>Heat budget</subject><subject>Heat flux</subject><subject>Heat transfer</subject><subject>Hydrodynamic models</subject><subject>Hydrodynamics</subject><subject>Inflow</subject><subject>Lakes</subject><subject>Monitoring systems</subject><subject>Monitoring/Environmental Analysis</subject><subject>Net radiation</subject><subject>Numerical models</subject><subject>Outflow</subject><subject>Oxygen</subject><subject>Radiation balance</subject><subject>Retention time</subject><subject>Sensible heat</subject><subject>Simulation</subject><subject>Summer</subject><subject>Thermal structure</subject><subject>Three dimensional models</subject><subject>Tributaries</subject><subject>Water inflow</subject><subject>Water outflow</subject><subject>Water quality</subject><subject>Water temperature</subject><subject>Water 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3D numerical modeling of the links between hydrodynamics, dissolved oxygen, and water temperature of a northern rural-urban shallow lake with two distinct basins</title><author>Hosseini-Sadabadi, Seyed Abbas ; Rousseau, Alain N. ; Sadeghian, Amir ; Foulon, Etienne ; Behmel, Sonja</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c352t-3977b624fcb904fc0622468f65a21fc86c6a0985a24eb9469b8e3b231015a9763</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Algae</topic><topic>Annual cycles</topic><topic>Annual variations</topic><topic>Aquatic ecosystems</topic><topic>Aquatic life</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic><topic>Basins</topic><topic>Cyanobacteria</topic><topic>Dissolved oxygen</topic><topic>Drinking water</topic><topic>Earth and Environmental 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Model outputs of T and DO corroborate observations at five monitoring stations within the lake. Simulated results indicated annual cycles of turnovers and stratifications and different behaviors for the deep and shallow basins. For the simulated years, the deep basin was stratified in summer and winter, while the shallow basin was mostly mixed throughout the year. The lake heat budget indicates that during summer with a long retention time, the thermal structure of the lake is principally controlled by net radiation, latent, and sensible heat fluxes. For the rest of the year, the inflow (from the main tributary, the Des Hurons River) and outflow are the main drivers of the lake’s thermal structure.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><doi>10.1007/s10661-023-11744-2</doi><tpages>1</tpages></addata></record> |
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subjects | Algae Annual cycles Annual variations Aquatic ecosystems Aquatic life Atmospheric Protection/Air Quality Control/Air Pollution Basins Cyanobacteria Dissolved oxygen Drinking water Earth and Environmental Science Ecology Ecotoxicology Enthalpy Environment Environmental Management Environmental monitoring Fluid mechanics Heat budget Heat flux Heat transfer Hydrodynamic models Hydrodynamics Inflow Lakes Monitoring systems Monitoring/Environmental Analysis Net radiation Numerical models Outflow Oxygen Radiation balance Retention time Sensible heat Simulation Summer Thermal structure Three dimensional models Tributaries Water inflow Water outflow Water quality Water temperature Water treatment |
title | A 3D numerical modeling of the links between hydrodynamics, dissolved oxygen, and water temperature of a northern rural-urban shallow lake with two distinct basins |
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