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Valeo, C
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Valeo, C
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Valeo, C
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Canadian Journal of Civil Engineering
Large-scale distributed watershed modelling for reservoir operations in cold boreal regions
General Environmental Science
Civil and Structural Engineering
author_sort st. laurent, m e
spelling St. Laurent, M E Valeo, C 0315-1468 1208-6029 Canadian Science Publishing General Environmental Science Civil and Structural Engineering http://dx.doi.org/10.1139/l06-142 <jats:p> The macroscale deterministic hydrologic model, SLURP, was modified and tested on two large watersheds in northern Manitoba, the Taylor River watershed (899 km<jats:sup>2</jats:sup>) and the upper Burntwood River watershed (6959 km<jats:sup>2</jats:sup>). Calibration and validation of the model on both watersheds between 1985 and 2000 identified a number of model deficiencies and recommendations for improvement. Date-dependent snowmelt rates were replaced with a single constant snowmelt rate, helping to decrease the parameterization of the model. A snowpack temperature deficit model was also incorporated to simulate the effects of snow ripening. These two modifications provided the modelling flexibility needed to control the timing of initial snowmelt and the rate of snowmelt. Annual spring freshet lasts roughly 2 weeks in this region; however, improved model performance was observed well beyond the spring freshet period. These modifications also provided a better representation of the physical processes that delay snowmelt once the air temperature exceeds 0 °C.Key words: frozen ground, boreal forest, hydrological modelling, snow ripening, snowmelt. </jats:p> Large-scale distributed watershed modelling for reservoir operations in cold boreal regions Canadian Journal of Civil Engineering
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title Large-scale distributed watershed modelling for reservoir operations in cold boreal regions
title_unstemmed Large-scale distributed watershed modelling for reservoir operations in cold boreal regions
title_full Large-scale distributed watershed modelling for reservoir operations in cold boreal regions
title_fullStr Large-scale distributed watershed modelling for reservoir operations in cold boreal regions
title_full_unstemmed Large-scale distributed watershed modelling for reservoir operations in cold boreal regions
title_short Large-scale distributed watershed modelling for reservoir operations in cold boreal regions
title_sort large-scale distributed watershed modelling for reservoir operations in cold boreal regions
topic General Environmental Science
Civil and Structural Engineering
url http://dx.doi.org/10.1139/l06-142
publishDate 2007
physical 525-538
description <jats:p> The macroscale deterministic hydrologic model, SLURP, was modified and tested on two large watersheds in northern Manitoba, the Taylor River watershed (899 km<jats:sup>2</jats:sup>) and the upper Burntwood River watershed (6959 km<jats:sup>2</jats:sup>). Calibration and validation of the model on both watersheds between 1985 and 2000 identified a number of model deficiencies and recommendations for improvement. Date-dependent snowmelt rates were replaced with a single constant snowmelt rate, helping to decrease the parameterization of the model. A snowpack temperature deficit model was also incorporated to simulate the effects of snow ripening. These two modifications provided the modelling flexibility needed to control the timing of initial snowmelt and the rate of snowmelt. Annual spring freshet lasts roughly 2 weeks in this region; however, improved model performance was observed well beyond the spring freshet period. These modifications also provided a better representation of the physical processes that delay snowmelt once the air temperature exceeds 0 °C.Key words: frozen ground, boreal forest, hydrological modelling, snow ripening, snowmelt. </jats:p>
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author St. Laurent, M E, Valeo, C
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author_sort st. laurent, m e
container_issue 4
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container_title Canadian Journal of Civil Engineering
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description <jats:p> The macroscale deterministic hydrologic model, SLURP, was modified and tested on two large watersheds in northern Manitoba, the Taylor River watershed (899 km<jats:sup>2</jats:sup>) and the upper Burntwood River watershed (6959 km<jats:sup>2</jats:sup>). Calibration and validation of the model on both watersheds between 1985 and 2000 identified a number of model deficiencies and recommendations for improvement. Date-dependent snowmelt rates were replaced with a single constant snowmelt rate, helping to decrease the parameterization of the model. A snowpack temperature deficit model was also incorporated to simulate the effects of snow ripening. These two modifications provided the modelling flexibility needed to control the timing of initial snowmelt and the rate of snowmelt. Annual spring freshet lasts roughly 2 weeks in this region; however, improved model performance was observed well beyond the spring freshet period. These modifications also provided a better representation of the physical processes that delay snowmelt once the air temperature exceeds 0 °C.Key words: frozen ground, boreal forest, hydrological modelling, snow ripening, snowmelt. </jats:p>
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spelling St. Laurent, M E Valeo, C 0315-1468 1208-6029 Canadian Science Publishing General Environmental Science Civil and Structural Engineering http://dx.doi.org/10.1139/l06-142 <jats:p> The macroscale deterministic hydrologic model, SLURP, was modified and tested on two large watersheds in northern Manitoba, the Taylor River watershed (899 km<jats:sup>2</jats:sup>) and the upper Burntwood River watershed (6959 km<jats:sup>2</jats:sup>). Calibration and validation of the model on both watersheds between 1985 and 2000 identified a number of model deficiencies and recommendations for improvement. Date-dependent snowmelt rates were replaced with a single constant snowmelt rate, helping to decrease the parameterization of the model. A snowpack temperature deficit model was also incorporated to simulate the effects of snow ripening. These two modifications provided the modelling flexibility needed to control the timing of initial snowmelt and the rate of snowmelt. Annual spring freshet lasts roughly 2 weeks in this region; however, improved model performance was observed well beyond the spring freshet period. These modifications also provided a better representation of the physical processes that delay snowmelt once the air temperature exceeds 0 °C.Key words: frozen ground, boreal forest, hydrological modelling, snow ripening, snowmelt. </jats:p> Large-scale distributed watershed modelling for reservoir operations in cold boreal regions Canadian Journal of Civil Engineering
spellingShingle St. Laurent, M E, Valeo, C, Canadian Journal of Civil Engineering, Large-scale distributed watershed modelling for reservoir operations in cold boreal regions, General Environmental Science, Civil and Structural Engineering
title Large-scale distributed watershed modelling for reservoir operations in cold boreal regions
title_full Large-scale distributed watershed modelling for reservoir operations in cold boreal regions
title_fullStr Large-scale distributed watershed modelling for reservoir operations in cold boreal regions
title_full_unstemmed Large-scale distributed watershed modelling for reservoir operations in cold boreal regions
title_short Large-scale distributed watershed modelling for reservoir operations in cold boreal regions
title_sort large-scale distributed watershed modelling for reservoir operations in cold boreal regions
title_unstemmed Large-scale distributed watershed modelling for reservoir operations in cold boreal regions
topic General Environmental Science, Civil and Structural Engineering
url http://dx.doi.org/10.1139/l06-142