基于复杂地形的低空风切变风场仿真检测

    Simulation and detection of low-altitude wind shear with complex terrain

    • 摘要: 低空风切变是指在较低高度内的近地面大气层中,风速或风向在水平或垂直方向上发生显著变化的现象。这种变化是很突然、强烈的,尤其在起飞和降落阶段造成严重的安全威胁,极易引发严重的坠机事故。因此对风切变实现准确的检测变得十分重要。但鉴于低空风切变的突发性、短时性以及不易探测性等,使得真实的风场数据难以直接获取,目前一般多采用仿真数据。本文在流体力学数值仿真方法基础上加入真实的地形数据,利用真实地形数据约束风切变风场仿真边界条件,获得了复杂地形环境下的低空风切变风场仿真数据,然后利用稀疏恢复的方法来实现地杂波的抑制并对风切变风速度进行估计。实验证明,本文方法获得的风场数据更能体现复杂地形环境对风切变风场的影响,地杂波的距离依赖性也更加明显。

       

      Abstract: Low-level wind shear is a phenomenon in which the wind speed or direction changes significantly in the horizontal or vertical direction in the near-surface atmosphere at lower altitudes. This change is very sudden and strong, especially during the take-off and landing stage, which poses a serious safety threat and can easily lead to serious crash accidents. However, due to the suddenness, short time and undetectability of low-level wind shear, it is difficult to obtain real wind field data directly, so simulation data is generally used at present. In this paper, real terrain data is added to the fluid dynamics numerical simulation method, and the real terrain data is used to constrain the simulation boundary conditions of wind shear wind field, and the simulation data of low-altitude wind shear wind field under complex terrain environment is obtained. Then, the sparse restoration method is used to suppress ground clutter and estimate wind shear wind velocity. Experimental results show that the wind field data obtained by this method can better reflect the influence of complex terrain environment on wind shear field, and the distance dependence of ground clutter is more obvious.
       

       

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