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Civil-Comp Proceedings
ISSN 1759-3433 CCP: 104
PROCEEDINGS OF THE SECOND INTERNATIONAL CONFERENCE ON RAILWAY TECHNOLOGY: RESEARCH, DEVELOPMENT AND MAINTENANCE Edited by: J. Pombo
Paper 33
Numerical Simulation of the Aerodynamic Behavior of High Velocity Trains under Synthetic Crosswinds of Different Shear and Turbulence Characteristics J. García1, J. Muñoz1, A. Jiménez2, E. Migoya1 and A. Crespo1
1Industrial Applied Fluid Mechanics Research Group, Department of Energy and Fluid Mechanics Engineering, Polytechnic University of Madrid, Spain
, "Numerical Simulation of the Aerodynamic Behavior of High Velocity Trains under Synthetic Crosswinds of Different Shear and Turbulence Characteristics", in J. Pombo, (Editor), "Proceedings of the Second International Conference on Railway Technology: Research, Development and Maintenance", Civil-Comp Press, Stirlingshire, UK, Paper 33, 2014. doi:10.4203/ccp.104.33
Keywords: train aerodynamics, cross wind, atmospheric turbulence.
Summary
A numerical simulation of the aerodynamic behavior of high-speed trains under
synthetic crosswinds at a 90° yaw angle is presented. The train geometry is the
aerodynamic train model (ATM). Flow description based on numerical simulations
is obtained using large eddy simulation (LES) and the commercial code ANSYS-Fluent
V14.5. A crosswind whose averaged velocity and turbulence characteristics
change with distance to the ground is imposed. Turbulent fluctuations that vary
temporally and spatially are simulated with TurbSim code. The crosswind boundary
condition is calculated for the distance the train runs during a simulation period. The
inlet streamwise velocity boundary condition is generated using Taylor's frozen
turbulence hypothesis. The model gives a time history of the force and moments
acting on the train; this includes averaged values, standard deviations and extreme
values. Of particular interest are the spectra of the forces and moments, and the
admittance spectra. For comparison, results obtained with LES and a uniform wind
velocity fluctuating in time, and results obtained with Reynolds averaged Navier
Stokes equations (RANS), and the averaged wind conditions, are also presented.
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