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Discontinuous Shallow Flow
A Numerical Method for Discontinuous Shallow Flow Fritz R. Fiedler University of Idaho Department of Civil Engineering
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Model Objectives Solve 2-D hydrodynamic flow equations
surface flow, rainfall, infiltration stiff hyperbolic equations non-linear source term Applications rainfall-runoff process wetlands flood plains
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Overland Flow
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Microtopography
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Equations
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Numerical Challenges Non-linear hyperbolic system Strong source terms
(equations stiff when h~0) Small depths / dry areas Large gradients Discontinuous flow regime
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Vector Form
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Vector Form
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Approach Select basic numerical scheme
Modify basic scheme to address problem-specific challenges Develop algorithm Develop code Test Iterate? (start simple)
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MacCormack Scheme Predictor, Backward Difference
Corrector, Forward Difference
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Split MacCormack Scheme
Lx1 Operator:
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Friction Slope: stiff!
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Friction Slope: Point-Implicit Treatment
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Convective Acceleration Upwinding
For the Lx1 operator: If flow is in the -x direction (j+1 to j)
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Smoothing Function
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Lateral Inflow and Infiltration
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Algorithm Input Define grid Initialize Solve time loop
compute lateral inflow (Newton’s Method) compute h, p, q output?
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Computer Code do 102 j=1,Nx-1 delh1(j,k) = - dtohx*(pc(j,k)-pc(j-1,k))+dt*0.5*re(j,k) delp1(j,k) = - D(j,k)*dtohx* & (convacc(j,k) + g*hc(j,k)**2 - g*hc(j-1,k)**2) & D(j,k)*dt * & ( g*(hc(j,k)+hc(j-1,k))*(z(j,k)-z(j-1,k))/hx & Ko*0.01*pc(j,k)/8./hc(j,k)**2 & pc(j,k)/hc(j,k)*re(j,k) ) & D(j,k)*dt/hx**2*eps1*(pc(j-1,k)-2.*pc(j,k)+pc(j+1,k)) delq1(j,k) = - dtohx* & ( pc(j,k)*qc(j,k)/hc(j,k) & pc(j-1,k)*qc(j-1,k)/hc(j-1,k) ) & dt/hx**2*eps1*(qc(j-1,k)-2.*qc(j,k)+qc(j+1,k)) continue
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Comparative Numerical Examples
Dam Break Problem Published results Physical Model Results
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Dam Break Problem
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Kinematic Wave Solution
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Microtopographic Surface
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Overland Flow Depths
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Flow Depths and Velocity
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Flow Channels
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Overland Flow Depths
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Cumulative Infiltration
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Simulated vs. Experimental
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