海洋模型输出的降维:在卫星图像运动估计中的应用

I. Herlin, E. Huot
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引用次数: 1

摘要

描述海洋表面动力学的运动场存在于高维矢量空间中。因此,从卫星图像中估计它们需要大量的计算资源。降维问题,即在这些高维空间中确定具有代表性的低维结构,对于任何需要实时或短期结果的应用都是非常重要的。适当的阶数分解允许确定这样的运动场的子空间,在这些子空间上可以以较低的复杂性评估估计。利用演化方程在该子空间上的伽辽金投影得到了一个简化模型。通过将观测到的图像序列与简化后的模型相同化来估计运动。本文描述了如何从海洋模式输出的数据库中导出约简空间,并解释了如何从卫星序列中估计地表环流。给出了NOAA-AVHRR传感器在黑海盆地获取的图像的结果。
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Dimensionality reduction on ocean model's outputs: Application to motion estimation on satellite images
Motion fields describing the ocean surface dynamics live in vectorial spaces of high dimension. Consequently, their estimation from satellite images requires huge computational resources. The issue of dimensionality reduction, that is the determination of representative low dimensional structures in these high dimensional spaces, is of major importance for any application that demands real-time or short-term results. Proper Order Decomposition allows to determine such sub-space of motion fields on which estimation may be assessed with reduced complexity. A reduced model is obtained by Galerkin projection of evolution equations on this subspace. Motion is estimated by assimilating the observed image sequence with the reduced model. The paper describes how to derive the reduced space from a database of ocean model's outputs and explains how to estimate surface circulation from satellite sequences. Results are given on images acquired on the Black Sea basin by NOAA-AVHRR sensors.
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