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A Consistent Spatio-temporal Motion Estimator for Atmospheric Layers

机译:大气层的一致时空运动估计器

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摘要

In this paper, we address the problem of estimating mesoscale dynamics of atmospheric layers from satellite image sequences. Relying on a physically sound vertical decomposition of the atmosphere into layers, we propose a dense motion estimator dedicated to the extraction of multi-layer horizontal wind fields. This estimator is expressed as the minimization of a global function including a data term and a spatio-temporal smoothness term. A robust data term relying on shallow-water mass conservation model is proposed to fit sparse observations related to each layer. A novel spatio-temporal regularizer derived from shallow-water momentum conservation model is proposed to enforce a temporal consistency of the solution along the sequence time range. These constraints are combined with a robust second-order regularizer preserving divergent and vorticity structures of the flow. In addition, a two-level motion estimation scheme is proposed to overcome the limitations of the multiresolution incremental scheme when capturing the dynamics of fine mesoscale structures. This alternative approach relies on the combination of correlation and optical-flow observations. An exhaustive evaluation of the novel method is first performed on a scalar image sequence generated by Direct Numerical Simulation of a turbulent bi-dimensional flow and then on a Meteosat infrared image sequence.
机译:在本文中,我们解决了根据卫星图像序列估算大气层中尺度动力学的问题。依靠大气的垂直物理分解成多层,我们提出了一种密集运动估计器,专用于多层水平风场的提取。该估计器表示为包括数据项和时空平滑项的全局函数的最小化。提出了一个依赖浅水质量守恒模型的鲁棒数据项,以适应与每一层有关的稀疏观测。提出了一种从浅水动量守恒模型导出的新型时空正则化函数,以在序列时间范围内增强解的时间一致性。这些约束条件与健壮的二阶正则化函数结合在一起,可保留流的发散和涡度结构。此外,提出了一种两级运动估计方案,以克服在捕获精细中尺度结构的动力学时多分辨率增量方案的局限性。这种替代方法依赖于相关性和光流观测的结合。首先对湍流二维流的直接数值模拟生成的标量图像序列进行详尽评估,然后对Meteosat红外图像序列进行详尽评估。

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