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Subtask 1.6.2 High Resolution Coastal Modelling. APAT Italian Agency for Environmental Protection. Francesco Lalli Luca Liberti. The Continuous Depth-Averaged Model * * * Turbulence Modeling: = 0 + t t = C H u Fischer (1973), Nezu (1996). The Discrete Model
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Subtask 1.6.2 High Resolution Coastal Modelling APAT Italian Agency for Environmental Protection Francesco Lalli Luca Liberti
The Continuous Depth-Averaged Model * * * Turbulence Modeling: = 0 + t t = C H uFischer (1973), Nezu (1996)
The Discrete Model • § Primitive Equations • § Finite Difference (Le and Moin, 1991) • Þ staggered grid • Þ time marching: 3rd order Runge-Kutta • Þ spatial derivatives: explicit 2nd order centered schemes • convective terms: SMART scheme (Gaskell & Lau, 1988) • § Complex Geometries: boundary body forces approach (Fadlun et al, 2000)
SIMPLE SHAPED CHANNEL HARBOUR: TIME-AVERAGED NUMERICAL SOLUTION
Pescara Harbor (Adriatic Sea, Italy) BREAKWATER JETTY MARINA PESCARA RIVER
BREAKWATER ENVIRONMENTAL EFFECTS Temperature Field
BAROTROPIC JET: PESCARA HARBOUR MODEL (horizontal scale 1:1000, vertical scale 1:100)
BAROCLINIC JET: PESCARA HARBOUR MODEL (horizontal scale 1:1000, vertical scale 1:100)
Wave-submerged barrier interaction: rip current generation (wave elevation)
Wave-submerged barrier interaction: rip current generation (velocity vectors)
Wave-submerged barrier interaction: rip current generation (vorticity)
Snapshot of the flow field: velocity vectors. Mala Neretva flow rate=72 m3/sec Neretva flow rate=156 m3/sec
Flow in a simple-shaped channel harbor Numerical Solution Re = UL/ = 100 Numerical Solution Re = UL/ = 300