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Reconstruction of Ocean Surface Maps by the Method of Local Spline Approximation with Chaotically Located Nodes

机译:节点位于混沌位置的局部样条逼近法重建海面地图

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The application of the local spline approximation method in for obtaining 2D or 3D maps of the anomalies of the sea surface dynamic topography domains with nonuniformly distributed initial information nodes is considered. The reconstruction of various stationary surfaces and surfaces changing with time over a period of 24 h is simulated. To reconstruct maps of the anomalies of the sea surface dynamic topography, the data of only one repeat cycle of the TOPEX/POSEIDON (T/P) satellite were used. The surface-reconstruction quality is estimated by calculating residual and other errors. The minimum spatial size of irregularities that can be reconstructed using this method of processing the altimetry data is obtained. The maps of an anomaly of the sea-surface topography plotted using the actual altimetry data from the T/P satellite are presented as an example demonstrating the efficiency of this technique.
机译:考虑了局部样条逼近方法在获得初始信息节点不均匀分布的海面动态地形域异常的2D或3D地图中的应用。模拟了各种固定表面的重建以及在24小时内随时间变化的表面。为了重建海面动态地形的异常图,仅使用了TOPEX / POSEIDON(T / P)卫星的一个重复周期的数据。通过计算残差和其他误差来估算表面重建质量。获得了可以使用这种处理测高数据的方法重建的不规则性的最小空间大小。以使用来自T / P卫星的实际测高数据绘制的海面地形异常图为例,展示了该技术的效率。

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