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Runoff Overview Tom Hopson
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Basic runoff processes
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Role in Flood Prediction Process
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General Soil Water Processes
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General Runoff Terms
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Surface Runoff
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Infiltration Excess Overland Flow
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Saturation Excess Overland Flow
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Interflow
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Transmissivity Feedback
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Soil-Bedrock Interface
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Groundwater Ridging
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Pre-Event Water
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Contributing Area and Runoff Volume
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Basin Size and Runoff Timing
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Basin Shape
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Stream Meanders
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Basin Slope
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Soil Properties
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In Depth: Soil Formation Processes
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Soil Texture Classification
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Soil Composition
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Soil Profile
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Surface Properties
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Runoff Modeling Concepts
-lumped -semi-distributed -distributes
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Complex Hydrologic Models
For forecast applications, adding complexity not always warranted: -limited observations to constrain parameters -run the risk of over-calibration
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Lumped Modeling Semi-Distributed Modeling
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Distributed Modeling -Don’t precisely capture watershed due to discretization -better capture forcing spatial variability and response
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Distributed modeling methods allow modeling of smaller and smaller basins. They also allow computation of more realistic runoff within a basin. Flash flood forecasts, for example, have improved with the implementation of distributed models. Distributed models do however require more complex and more high-resolution data, introducing more uncertainty.
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