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Modified SWAT Model for Cold Climate of Canada Rouge River Modified SWAT Model for Cold Climate of Canada Application: Rouge River Watershed Masoud Asadzadeh Wanhong Yang & Yongbo Liu Luis Leon & William Booty Ram Yerubandi, Craig McCrimmon, Issac Wong, and Phil Fong
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Simulate the Current State of the Rouge River Watershed (Base Case) Soil Type Land-Use Management Operations Observed Climate Data Observed Flow and Water Quality Data Estimate the Impact of Increasing the Forest Land-Use (Reforestation) Increase the Forest Land-Use Compare Base Case and Reforestation Scenarios: Simulated Flow, Water Quality Objectives Case Study Methods Results Conclusions
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Rouge River Watershed Objectives Case Study Methods Results Conclusions TRCA watershed maps: http://trca.on.ca/the-living-city/watersheds/http://trca.on.ca/the-living-city/watersheds/ Scholars GeoPortal website: http://geo2.scholarsportal.info/http://geo2.scholarsportal.info/ Little Rouge at Reesor Road Main Rouge near 14 th Avenue Main Rouge at Twyn Rivers Drive
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Rouge River Watershed Objectives Case Study Methods Results Conclusions Data from Canadian Soil Information Service (CanSIS) Version 3
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Rouge River Watershed Objectives Case Study Methods Results Conclusions Data and map is provided by TRCA and represents 2005 conditions Hay38 Corn30 Soybean22 Winter Wheat10
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CanSWAT Snow Redistribution: Snow can redistribute between land-use classes based on: Wind direction Slope and curvature along the wind direction Elevation Snowmelt under Frozen Soil Condition: Modified CNfrz based on SW of each layer of the soil Added soil erodibility factor for snowmelt events Added user defined nutrient enrichment ratios, nitrate percolation coefficient, and P soil partitioning coefficient for snowmelt events. Objectives Case Study Methods Results Conclusions
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Calibration Objectives Sum of Absolute Error Percent Bias in High Flow Percent Bias in Low Flow Percent Bias in Mid-Range Flow Objectives Case Study Methods Results Conclusions
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PA-DDS Objectives Case Study Methods Results Conclusions Perturb current ND solution Update ND solutions Continue? STOP New solution is ND? Pick the New solution Pick a ND solution Initialize starting solutions Y N Create ND-solution set Y N
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Base Case Water Balance Components Annual Average Estimated by Water Balance Studies in the Past CanSWAT Precipitation (mm) 840 - 870837 Snowfall (mm) 126 - 130102 Evapotranspiration (mm) 520 - 540477 Runoff (mm) 320 - 330351 Surface Flow (mm) 189 - 196209 Objectives Case Study Methods Results Conclusions
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Base Case Objectives Case Study Methods Results Conclusions
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Base Case Objectives Case Study Methods Results Conclusions
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Base Case Objectives Case Study Methods Results Conclusions
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Base Case Objectives Case Study Methods Results Conclusions
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Base Case Objectives Case Study Methods Results Conclusions
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Base Case Objectives Case Study Methods Results Conclusions
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Base Case Objectives Case Study Methods Results Conclusions
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Base Case Objectives Case Study Methods Results Conclusions
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Base Case Objectives Case Study Methods Results Conclusions
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Reforestation Objectives Case Study Methods Results Conclusions
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Reforestation Objectives Case Study Methods Results Conclusions
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Reforestation Objectives Case Study Methods Results Conclusions
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Reforestation Rouge River Watershed Outlet Base CaseReforestation% difference TSS (mg/l) 218185 ↓ 15.1↓ TP (mg/l) 0.2870.280 ↓ 2.5 ↓ TN (mg/l) 1.2671.223 ↓ 3.5 ↓ High Flow (cms) 38.535.4 ↓ 8.0 ↓ Low Flow (cms) 1.001.01 ↑ 1.0 ↑ Objectives Case Study Methods Results Conclusions
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Rouge River watershed is modelled with detailed information about the soil type, land- use, and land management operations. CanSWAT is calibrated to adequately simulate flow and water quality constituents. The calibrated model is a good representation of the rainfall-runoff relationship in the Rouge River watershed. Reforestation can reduce sediments and nutrients delivered into the Lake Ontario from the watershed. Objectives Case Study Methods Results Conclusions
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Thank You Objectives Case Study Methods Results Conclusions
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