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Runoff in MIKE-SWMM Melissa Figurski
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Subroutine Schematic OVRLND subroutine does runoff.
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Surface Flow Routing Elements
Subcatchment (overland flow) Channel (trapezoidal/parabolic channel flow) Pipe (circular channel flow) Control Structures (weirs and orifices)
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Discretization “Mathematical abstraction of the physical drainage system” Turn basin into rectangles Fine vs. Coarse Discretization How the computer sees your basin. More on pg. 80
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Discretization
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Subcatchment Overview
Discretize basin into subcatchments Calculate runoff from each subcatchment Combine outflow from each subcatchment for total runoff Total runoff is computed through a
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Subcatchment Subareas
Three subareas in each subcatchment represent impervious w/ storage, impervious w/o storage, and previous w/ storage. Actually, subcatchment can consist entirely of one or more types of subareas. Width of impervious area is ratio of impervious area to total impervious area.
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Non-linear Reservoir d2 – d1 = i* + WCON [d1 + 0.5(d2 – d1) – dp]/5/3
Manning’s equation for flow. W is width of subcatchment. Non-linear eqn. from combination of Maning’s and continuity equation. Eqn. for time step – solve for d2 with Newton-Raphson method. Plug d2 into Manning’s equation for outflow in that period. i* = rainfall excess d2 – d1 = i* + WCON [d (d2 – d1) – dp]/5/3 Dt 1.49 W S1/2 WCON = – A n
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Reference Storm Water Management Model: Version 4, User’s Manual.
Section 4: Runoff Block, Appendix VI
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