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首页> 外文期刊>Pattern Recognition: The Journal of the Pattern Recognition Society >Motion analysis in oceanographic satellite images using multiscale methods and the energy cascade
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Motion analysis in oceanographic satellite images using multiscale methods and the energy cascade

机译:使用多尺度方法和能量级联的海洋卫星图像中的运动分析

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摘要

Motion analysis of complex signals is a particularly important and difficult topic, as classical Computer Vision and Image Processing methodologies, either based on some extended conservation hypothesis or regularity conditions, may show their inherent limitations. An important example of such signals are those coming from the remote sensing of the oceans. In those signals, the inherent complexities of the acquired phenomenon (a fluid in the regime of fully developed turbulence-FDT) are made even more fraught through the alterations coming from the acquisition process (sun glint, haze, missing data etc.). The importance of understanding and computing vector fields associated to motion in the oceans or in the atmosphere (e.g.: cloud motion) raises some fundamental questions and the need for derivating motion analysis and understanding algorithms that match the physical characteristics of the acquired signals. Among these questions, one of the most fundamental is to understand what classical methodologies (e.g.: such as the various implementations of the optical flow) are missing, and how their drawbacks can be mitigated. In this paper, we show that the fundamental problem of motion evaluation in complex and turbulent acquisitions can be tackled using new multiscale characterizations of transition fronts. The use of appropriate paradigms coming from Statistical Physics can be combined with some specific Signal Processing evaluation of the microcanonical cascade associated to turbulence. This leads to radically new methods for computing motion fields in these signals. These methods are first assessed on the results of a 3D oceanic circulation model, and then applied on real data.
机译:复杂信号的运动分析是一个特别重要且困难的主题,因为基于某些扩展的保护假设或规则性条件的经典计算机视觉和图像处理方法可能会显示其固有的局限性。这种信号的一个重要例子是来自海洋遥感的信号。在这些信号中,由于采集过程产生的变化(阳光闪烁,阴霾,数据丢失等),使得采集到的现象(在完全发展的湍流-FDT态下的流体)固有的复杂性更加紧张。了解和计算与海洋或大气中的运动(例如云运动)相关的矢量场的重要性提出了一些基本问题,并且需要推导运动分析和理解与所采集信号的物理特征相匹配的算法。在这些问题中,最根本的问题之一就是要了解缺少哪些经典方法(例如:光流的各种实现),以及如何减轻它们的缺点。在本文中,我们表明,可以使用过渡前沿的新多尺度表征来解决复杂和湍流采集中运动评估的基本问题。可以将来自统计物理学的适当范例的使用与对与湍流相关的微经典级联的某些特定信号处理评估结合起来。这导致了用于计算这些信号中运动场的全新方法。首先根据3D海洋环流模型的结果评估这些方法,然后将其应用于实际数据。

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