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A Variational Stereo Method for the Three-Dimensional Reconstruction of Ocean Waves

机译:海浪三维三维重构的变分立体方法

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We develop a novel remote sensing technique for the observation of waves on the ocean surface. Our method infers the 3-D waveform and radiance of oceanic sea states via a variational stereo imagery formulation. In this setting, the shape and radiance of the wave surface are given by minimizers of a composite energy functional that combines a photometric matching term along with regularization terms involving the smoothness of the unknowns. The desired ocean surface shape and radiance are the solution of a system of coupled partial differential equations derived from the optimality conditions of the energy functional. The proposed method is naturally extended to study the spatiotemporal dynamics of ocean waves and applied to three sets of stereo video data. Statistical and spectral analysis are carried out. Our results provide evidence that the observed omnidirectional wavenumber spectrum $S(k)$ decays as $k^{-2.5}$ is in agreement with Zakharov's theory (1999). Furthermore, the 3-D spectrum of the reconstructed wave surface is exploited to estimate wave dispersion and currents.
机译:我们开发了一种新颖的遥感技术,用于观察海面的波浪。我们的方法通过变体立体图像公式推断出3D波形和海洋海域的辐射度。在这种情况下,波表面的形状和辐射由复合能量函数的极小值给出,该函数将光度匹配项与涉及未知数平滑度的正则化项相结合。所需的海洋表面形状和辐射度是从能量函数的最佳条件得出的耦合偏微分方程组的解。该方法自然扩展到研究海浪的时空动态,并应用于三套立体声视频数据。进行统计和光谱分析。我们的结果提供了证据,表明观测到的全向波数谱$ S(k)$随$ k ^ {-2.5} $衰减而与Zakharov理论(1999年)一致。此外,利用重构波表面的3D光谱来估计波的色散和电流。

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