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Nonlinear Ocean Wave Reconstruction Algorithms Based on Simulated Spatiotemporal Data Acquired by a Flash LIDAR Camera

机译:基于闪光灯LIDAR摄像机时空数据的非线性海浪重构算法

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We report on the development of free surface reconstruction algorithms to predict ocean waves, based on spatial observations made with a high-frequency Flash light detection and ranging camera. We assume that the camera is mounted on a vessel, in a forward looking position, and is pointing at some distance ahead of its path yielding a sample of spatiotemporal wave elevation data. Because of the geometry, the density of measurement points gradually decreases (i.e., becomes sparse) with the distance to the camera. Free surface reconstruction algorithms were first developed and validated for linear 1-D and 2-D irregular surface models, whose amplitude coefficients are estimated on the basis of minimizing the mean square error of simulated surface elevations to measurements, over space and time (for a specified time initialization period). In the validation tests reported here, irregular ocean surfaces are generated on the basis of a directional Pierson-Moskowitz or Elfouhaily spectrum, and simulated LIDAR data sets are constructed by performing geometric intersections of laser rays with each generated surface. Once a nowcast of the ocean surface is estimated from the (simulated) LIDAR data, a forecast can be made of expected waves ahead of the vessel, for a time window that depends both on the initialization period and the resolved wavenumbers in the reconstruction. The process can then be repeated for another prediction window, and so forth. To reconstruct severe sea states, however, nonlinear effects must be included in the sea surface representation. This is done, here, by representing the ocean surface using the efficient Lagrangian choppy wave model .
机译:我们报告了基于使用高频闪光灯检测和测距相机进行的空间观测来预测海浪的自由表面重建算法的发展。我们假设摄像机安装在船只上,处于向前看的位置,并且指向其路径前方的某个距离,从而产生时空波高程数据样本。由于其几何形状,测量点的密度随着与相机的距离逐渐减小(即变得稀疏)。首先开发了自由表面重构算法,并针对线性一维和二维不规则表面模型进行了验证,该模型的幅值系数是根据在空间和时间上最小化模拟表面高程相对于测量值的均方误差来估算(指定的时间初始化周期)。在这里报告的验证测试中,不规则的海洋表面是根据定向Pierson-Moskowitz或Elfouhaily光谱生成的,并且模拟的LIDAR数据集是通过对每个生成的表面执行激光的几何相交来构造的。一旦从(模拟的)LIDAR数据估计了海面的临近预报,就可以对船前的预期波进行预测,其时间窗取决于初始化周期和重建中的解析波数。然后可以针对另一个预测窗口重复该过程,等等。但是,要重建严重的海况,必须在海面表示中包含非线性效应。这是通过使用有效的拉格朗日波涛起伏的海浪模型表示海洋表面来完成的。

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