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Large eddy simulation of aircraft wake vortices in a homogeneous atmospheric turbulence - Vortex decay and descent
Author(s) -
Jongil Han,
YuhLang Lin,
S. Pal Arya,
Fred Proctor
Publication year - 1999
Publication title -
38th aerospace sciences meeting and exhibit
Language(s) - English
Resource type - Conference proceedings
DOI - 10.2514/6.1999-756
Subject(s) - vortex , turbulence , physics , mechanics , wake , homogeneous isotropic turbulence , k epsilon turbulence model , wake turbulence , stratification (seeds) , exponential decay , turbulence kinetic energy , vortex stretching , vortex ring , meteorology , computational physics , direct numerical simulation , reynolds number , nuclear physics , seed dormancy , germination , botany , dormancy , biology
The effects of ambient turbulence on decay and descent of aircraft wake vortices are studied using a validated, three-dimensional, large-eddy simulation model. Numerical simulations are performed in order to isolate the effect of ambient turbulence on the wake vortex decay rate within a neutrally-stratified atmosphere. Simulations are conducted for a range of turbulence intensities, by injecting wake vortex pairs into an approximately homogeneous and isotropic turbulence field. The decay rate of the vortex circulation increases clearly with increasing ambient turbulence level, which is consistent with field observations. Based on the results from the numerical simulations, simple decay models are proposed as functions of dimensionless ambient turbulence intensity (n) and demisnionless time (T) for the circulation averaged over a range of radial distances. With good agreement with the numerical results, a Gaussian type of vortex decay model is proposed for weak turbulence, while an exponential type of vortex decay model can be applied for strong turbulence. A relationship for the vortex descent based on above vortex decay model is also proposed. Although the proposed models are based on simulations assuming neutral stratification, the model predictions are compared to Lidar vortex measurements observed during stable, neutral, and unstable atmospheric conditions. In the neutral and unstable atmospere, the model predictions appear to be in reasonable agreement with the observational data, while in the stably-stratified atmosphere, they largely underestimate the observed circulation decay with consistent overestimation of the observed vortex descent. The underestimation of vortex decay during stably-stratified conditions suggests that stratification has an important influence on vortex decay when ambient levels of turbulence are weak.

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