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Grant: Strategic Projects - Group

University of Waterloo

$284,070.00

Three dimensional hydrodynamic and ecological models for water quality problems in Lake Erie

EF 2007-08

Résumé
Billions of dollars have been spent on the control of nutrient loading to Lake Erie in the U.S. and Canada with the elimination of deep water hypoxia (low oxygen levels) in the central basin of the lake an important goal. In spite of improvements in chlorophyll and phosphorus levels in offshore lake waters, hypoxia appears to have worsened in recent years. There are several hypotheses for the cause of this, including changing climatic conditions, changes in nutrient input from rivers, and the effects of non-native mussels which invaded Lake Erie in the 1980s.Deep water hypoxia occurs in the lower layer of the lake, called the hypolimnion, which lies beneath a thin layer of rapid temperature change with depth called the metalimnion. The metalimnion represents a barrier for the downward flux of oxygen. In recent years it has become appreciated that breaking internal waves in the metalimnion are an important mechanism for this downward flux. This is one of several ways in which physical processes in the lake have an impact on biological and chemical processes.In this research data will be used to validate a lake-scale hydrodynamic-biogeochemical numerical model which will then be used to demonstrate the implications of current hypotheses and to explore the possible implications of future climate change scenarios. In order to elucidate the role of breaking internal waves in the thermocline a field program will be conducted to obtain data with high temporal and spatial resolution. This will be the first such study in Lake Erie. Physical, chemical and biological measurements will be made enabling links between various processes to be made and to establish their role in the formation of hypoxic water. Lake-scale and high-resolution numerical simulations will be undertaken to provide a fuller picture of these important processes. This research will result in a synthesized picture of the role of large and small scale processes in the formation of deep water hypoxia and provide useful tools for the future management of this important lake, tools which can also be applied to other lakes.
Programme
Strategic Projects - Group
Emplacement
Ontario, Canada
Type de bénéficiaire
Academia
Type
Grant
Source
NSERC's Awards Data

Tel que publié

Application id
350475-2007
Name nom
Lamb, Kevin
Department département
Applied Mathematics
Organization id
33
Institution établissement
University of Waterloo
Province en
Ontario
Province fr
Ontario
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2007
Competition year année de concours
2007
Award amount
284070
Program id
STPGP
Program name en
Strategic Projects - Group
Program name fr
Projets stratégiques - De groupe
Group en
Research partnerships programs
Group fr
Programmes de partenariat
Committee code
1060
Committee name en
Strategic Projects Selection Panel - Environment B
Committee name fr
Comité de sélection des projets stratégiques - Environnement B
Area of application code
403
Area of application group en
Environment
Area of application group fr
Environnement
Area of application en
Inland waters
Area of application fr
Eaux intérieures
Research subject code
1501
Research subject group en
Environmental engineering
Research subject group fr
Génie de l'environnement
Research subject en
Water quality, pollution
Research subject fr
Qualité de l'eau, pollution
Partie
1
Nb partie
3
Application title
Three dimensional hydrodynamic and ecological models for water quality problems in Lake Erie
Keyword
NA
Application summary
Billions of dollars have been spent on the control of nutrient loading to Lake Erie in the U.S. and Canada with the elimination of deep water hypoxia (low oxygen levels) in the central basin of the lake an important goal. In spite of improvements in chlorophyll and phosphorus levels in offshore lake waters, hypoxia appears to have worsened in recent years. There are several hypotheses for the cause of this, including changing climatic conditions, changes in nutrient input from rivers, and the effects of non-native mussels which invaded Lake Erie in the 1980s.Deep water hypoxia occurs in the lower layer of the lake, called the hypolimnion, which lies beneath a thin layer of rapid temperature change with depth called the metalimnion. The metalimnion represents a barrier for the downward flux of oxygen. In recent years it has become appreciated that breaking internal waves in the metalimnion are an important mechanism for this downward flux. This is one of several ways in which physical processes in the lake have an impact on biological and chemical processes.In this research data will be used to validate a lake-scale hydrodynamic-biogeochemical numerical model which will then be used to demonstrate the implications of current hypotheses and to explore the possible implications of future climate change scenarios. In order to elucidate the role of breaking internal waves in the thermocline a field program will be conducted to obtain data with high temporal and spatial resolution. This will be the first such study in Lake Erie. Physical, chemical and biological measurements will be made enabling links between various processes to be made and to establish their role in the formation of hypoxic water. Lake-scale and high-resolution numerical simulations will be undertaken to provide a fuller picture of these important processes. This research will result in a synthesized picture of the role of large and small scale processes in the formation of deep water hypoxia and provide useful tools for the future management of this important lake, tools which can also be applied to other lakes.