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The NASA-Langley Wake Vortex Modelling Effort in Support of an Operational Aircraft Spacing System

机译:支持飞行器间隔系统的NASA-Langley尾涡建模工作

摘要

Two numerical modelling efforts, one using a large eddy simulation model and the other a numerical weather prediction model, are underway in support of NASA's Terminal Area Productivity program. The large-eddy simulation model (LES) has a meteorological framework and permits the interaction of wake vortices with environments characterized by crosswind shear, stratification, humidity, and atmospheric turbulence. Results from the numerical simulations are being used to assist in the development of algorithms for an operational wake-vortex aircraft spacing system. A mesoscale weather forecast model is being adapted for providing operational forecast of winds, temperature, and turbulence parameters to be used in the terminal area. This paper describes the goals and modelling approach, as well as achievements obtained to date. Simulation results will be presented from the LES model for both two and three dimensions. The 2-D model is found to be generally valid for studying wake vortex transport, while the 3-D approach is necessary for realistic treatment of decay via interaction of wake vortices and atmospheric boundary layer turbulence. Meteorology is shown to have an important affect on vortex transport and decay. Presented are results showing that wake vortex transport is unaffected by uniform fog or rain, but wake vortex transport can be strongly affected by nonlinear vertical change in the ambient crosswind. Both simulation and observations show that atmospheric vortices decay from the outside with minimal expansion of the core. Vortex decay and the onset three-dimensional instabilities are found to be enhanced by the presence of ambient turbulence.
机译:为了支持NASA的终端区生产力计划,正在进行两项数值建模工作,一项使用大型涡流仿真模型,另一项使用数值天气预报模型。大涡模拟模型(LES)具有气象框架,并且允许尾流涡流与侧风剪切,分层,湿度和大气湍流等环境相互作用。数值模拟的结果被用于协助开发可操作的尾涡旋飞机间隔系统的算法。正在调整中尺度天气预报模型,以提供终端区使用的风,温度和湍流参数的运行预测。本文介绍了目标和建模方法,以及迄今为止取得的成就。 LES模型将针对二维和三维提供仿真结果。发现2-D模型通常对于研究尾流涡流是有效的,而3-D方法对于通过尾流涡流和大气边界层湍流的相互作用进行衰减的现实处理是必需的。事实证明,气象学对涡旋的传播和衰减具有重要影响。呈现的结果表明,尾流涡流不受均匀的雾或雨的影响,但尾涡流受周围侧风的非线性垂直变化影响很大。模拟和观测结果均表明,大气涡旋从外部衰减,而核心膨胀最小。发现涡旋衰减和开始的三维不稳定性会因周围湍流的存在而增强。

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    Proctor Fred H.;

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  • 年度 1998
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