Flooding Overlay

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Revision as of 09:21, 28 June 2018 by Daniel2@tygron.com (talk | contribs) (Created page with "==2D Saint Venant equations== ∂l/∂t+∂du/∂x+∂dv/∂y=q_in ∂u/∂t+u ∂u/∂x+v ∂u/∂y+g ∂l/∂x+g u|u ⃗ |/(C^2 d)=0 ∂v/∂t+u ∂v/∂x+v ∂v/∂y+g ∂l...")
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2D Saint Venant equations

∂l/∂t+∂du/∂x+∂dv/∂y=q_in ∂u/∂t+u ∂u/∂x+v ∂u/∂y+g ∂l/∂x+g u|u ⃗ |/(C^2 d)=0 ∂v/∂t+u ∂v/∂x+v ∂v/∂y+g ∂l/∂y+g v|u ⃗ |/(C^2 d)=0 Where: d water depth (m + bottom) l water level (m + reference) u velocity in x-direction (m/s) v velocity in y-direction (m/s) qin lateral boundary condition (m/s) t time (s) g gravitation constant (9.80655 m/s2) C Chezy-coefficient (m1/2/s): C= d^(1/6)/n n Manning coefficient (s/m1/3) |u ⃗ | velocity magnitude: √(u^2+v^2 )


Explicit numerical scheme

The Tygron Engine Inundation module relies on an explicit finit volume method, taken from Kurganov and Petrova (2007). This scheme relies on a reconstruction of cell bottom, water level and velocity at the interfaces between computational cells as proposed by Lax and Wendroff (see Rezzolla, 2011). The reconstruction method, taken from Bolderman et all (2014) ensures numerical stability, especially at the wetting and drying front of a flood wave.

Computational time step

References