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Space-time ocean wave measurement using variational stereo vision systems

机译:使用变体立体视觉系统进行时空海浪测量

摘要

Remote sensing imaging systems for the measurement of oceanic sea states have recently attracted renovated attention. Imaging technology is economical, non-invasive and enables a better understanding of the space-time dynamics of ocean waves over an area rather than at selected point locations of previous monitoring methods (buoys, wave gauges, etc.). We present recent progress in space-time measurement of ocean waves using stereo vision systems on offshore platforms. Both traditional disparity-based systems and modern elevation-based ones are presented in a variational optimization framework: the main idea is to pose the stereoscopic reconstruction problem of the surface of the ocean in a variational setting and design an energy functional whose minimizer is the desired temporal sequence of wave heights. The functional combines photometric observations as well as spatial and temporal smoothness priors. Disparity methods estimate the disparity between images as an intermediate step toward retrieving the depth of the waves with respect to the cameras, whereas elevation methods estimate the ocean surface displacements directly in 3-D space. Both techniques are used to measure ocean waves from real data collected at offshore platforms in the Black Sea (Crimean Peninsula, Ukraine) and the Northern Adriatic Sea (Venice coast, Italy). Then, the statistical and spectral properties of the resulting observed waves are analyzed. We show the advantages and disadvantages of the presented stereo vision systems and discuss the improvement of their performance in critical issues such as the robustness of the camera calibration in spite of undesired variations of the camera parameters.
机译:用于测量海洋海况的遥感成像系统最近引起了人们的关注。成像技术是经济的,非侵入性的,可以更好地了解某个区域而不是先前的监视方法(浮标,波表等)的选定点位置处的海浪的时空动态。我们介绍了在海上平台上使用立体视觉系统对海浪进行时空测量的最新进展。在变分优化框架中介绍了传统的基于视差的系统和现代的基于高程的系统:主要思想是在变化的环境中提出海洋表面的立体重建问题,并设计所需的最小化能量函数波高的时间顺序。该功能结合了光度学观察以及先验的空间和时间平滑度。视差方法估计图像之间的视差,这是获取相对于摄像机的波深的中间步骤,而高程方法则直接估计3-D空间中的海洋表面位移。两种技术都用于从在黑海(克里米亚半岛,乌克兰)和北亚得里亚海(意大利威尼斯海岸)的近海平台收集的真实数据测量海浪。然后,分析所得观测波的统计和光谱特性。我们展示了所提出的立体视觉系统的优缺点,并讨论了在关键问题(例如摄像机标定的鲁棒性)方面的性能改进,尽管摄像机参数发生了不希望的变化。

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