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Scaling Analysis of Ocean Surface Turbulent Heterogeneities from Satellite Remote Sensing: Use of 2D Structure Functions

机译:卫星遥感海面湍流非均质性的尺度分析:二维结构函数的使用

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摘要

Satellite remote sensing observations allow the ocean surface to be sampled synoptically over large spatio-temporal scales. The images provided from visible and thermal infrared satellite observations are widely used in physical, biological, and ecological oceanography. The present work proposes a method to understand the multi-scaling properties of satellite products such as the Chlorophyll-a (Chl-a), and the Sea Surface Temperature (SST), rarely studied. The specific objectives of this study are to show how the small scale heterogeneities of satellite images can be characterised using tools borrowed from the fields of turbulence. For that purpose, we show how the structure function, which is classically used in the frame of scaling time series analysis, can be used also in 2D. The main advantage of this method is that it can be applied to process images which have missing data. Based on both simulated and real images, we demonstrate that coarse-graining (CG) of a gradient modulus transform of the original image does not provide correct scaling exponents. We show, using a fractional Brownian simulation in 2D, that the structure function (SF) can be used with randomly sampled couple of points, and verify that 1 million of couple of points provides enough statistics.
机译:通过卫星遥感观测,可以在较大的时空尺度上对海面进行同步采样。从可见光和热红外卫星观测中获得的图像广泛用于物理,生物和生态海洋学。目前的工作提出了一种了解卫星产品(例如叶绿素a(Chl-a)和海表温度(SST))的多尺度特性的方法,这种方法很少研究。这项研究的特定目标是展示如何使用从湍流领域借来的工具来表征小规模的卫星图像异质性。为此,我们展示了在缩放时间序列分析框架中经典使用的结构函数如何也可以在2D中使用。该方法的主要优点是可以应用于缺少数据的过程映像。基于模拟和真实图像,我们证明原始图像的梯度模量变换的粗粒度(CG)无法提供正确的缩放指数。我们显示,使用2D分数布朗仿真,可以将结构函数(SF)与随机采样的几个点一起使用,并验证一百万个点对提供了足够的统计信息。

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