首页> 外文学位 >A SPATIAL MODEL OF WIND SHEAR AND TURBULENCE FOR FLIGHT SIMULATION (MONTE CARLO, SIMULATION, MICROBURST).
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A SPATIAL MODEL OF WIND SHEAR AND TURBULENCE FOR FLIGHT SIMULATION (MONTE CARLO, SIMULATION, MICROBURST).

机译:飞行模拟风切变和湍流的空间模型(蒙特卡洛,模拟,微暴)。

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摘要

A three dimensional model which combines measurements of wind shear in the real atmosphere with three-dimensional Monte Carlo simulated turbulence was developed. The measurement of three-dimensional wind shear is a recent development. Measurements were made on a rather coarse ((TURN) 200 m) grid scale so that high frequency, short length scale turbulence information was not included. Some of the missing frequencies are important to aircraft response and hence for flight simulation. The missing turbulence must be added to the wind shear measurements. The spatial model adds three-dimensional, Monte-Carlo simulated turbulence conforming to the von Karman model. The turbulence was generated in the frequency domain and transformed to the space domain using Fast Fourier Transform techniques. The resulting turbulence is three-dimensional and contains lateral and vertical as well as longitudinal correlations associated with isotropic turbulence. The resulting Gaussian, isotropic turbulence is multiplied by a spatially varying gust intensity and added to the wind shear data set winds. The resulting simulated wind field is nonisotropic, non-Gaussian, and nonlinear as are winds in the real atmosphere. Previous turbulence simulations were either one-dimensional or accounted for two- or three-dimensionality in an artificial way. With the present model, the wind field over the body of an aircraft can be simulated and all aerodynamic loads and moments calculated. The inclusion of three-dimensional variation of winds and turbulence is believed to be a significant advance over previous wind simulation models.
机译:建立了三维模型,该模型将真实大气中风切变的测量结果与三维蒙特卡洛模拟湍流相结合。三维风切变的测量是最近的发展。测量是在相当粗糙的((转向)200 m)网格规模上进行的,因此不包括高频短长度尺度的湍流信息。一些丢失的频率对于飞机的响应并因此对于飞行仿真很重要。必须将缺失的湍流添加到风切变测量中。空间模型添加了符合von Karman模型的三维蒙特卡洛模拟湍流。湍流在频域中生成,并使用快速傅立叶变换技术转换为空间域。产生的湍流是三维的,包含与各向同性湍流相关的横向和纵向以及纵向相关性。所得的高斯各向同性湍流乘以空间变化的阵风强度,并添加到风切变数据集风中。生成的模拟风场与实际大气中的风一样,是非各向同性的,非高斯的和非线性的。以前的湍流模拟要么是一维的,要么是以人工方式考虑的二维或三维的。使用本模型,可以模拟飞机机体上的风场,并计算所有的空气动力学载荷和力矩。包含风和湍流的三维变化被认为是相对于以前的风仿真模型的重大进步。

著录项

  • 作者

    CAMPBELL, C. WARREN.;

  • 作者单位

    Colorado State University.;

  • 授予单位 Colorado State University.;
  • 学科 Plasma physics.
  • 学位 Ph.D.
  • 年度 1984
  • 页码 133 p.
  • 总页数 133
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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