Sentence examples for wind flow simulation from inspiring English sources

The purpose of this study is to evaluate the capabilities of the improved delayed detached eddy simulation (IDDES) model in a wind flow simulation.

The resulting wind flow simulation software is designed for use in an engineering workstation environment, in which, the new coupled scheme offers more efficient and improved computational effort.

The wind flow simulations have been performed by means of a mass-consistent model.

The present framework employs three-dimensional Reynolds Averaged Navier Stokes (RANS) equations along with multi-block approach and non-conformal meshes to perform wind flow simulations over such sites with complex geometry.

Bioclimatic considerations that involve solar radiation analysis and computational fluid dynamic (CFD -based wind flow simulations have been integrated into the parametriCFD -basedn order to explore the interaction of the geometry of the proposed buildings wind the solar exposure and the prevailing winds in the area throughout the year.

Validation of the wind-flow simulations is performed with Particle Image Velocimetry (PIV) measurements in a wind tunnel.

These results are compared with those from the wind tunnel flow simulations at a geometric scale ratio of 1/50.

The purpose is to obtain information that will aid in the reduction of hurricane wind damage to residential structures by providing input for wind tunnel and full-scale flow simulation experiments that assess wind loads on these structures under hurricane conditions.

Fig. 12 Electric potential in a weak solar wind magnetic field, obtained from the simulation run #4, at time t = 9.4 × 102ω-1 (60000 steps) when the solar wind flow has swept the simulation domain a little more than twice.

Fig. 11 (a) The electron density ne and (b) the electric potential ϕ for the reduced Debye length case λD = 0.125Ro, obtained from the simulation run #3 at time t = 9.0 × 102ω-1 (180000 steps) when the solar wind flow has swept the simulation domain twice.

This was first observed when higher order Godunov schemes with Riemann solvers were first applied to metreological simulations (which simulate wind flow in the earth's atmosphere) or to the shallow water equations (which simulate lake and ocean circulation) (Parés 2006).