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Front detection on satellite images based on wavelet and evidence theory: Application to the sea breeze fronts

机译:基于小波和证据理论的卫星图像前检测:在海风锋中的应用

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This paper is concerned with the detection of fronts in satellite images. We focus on some specific textured patterns of clouds that are visible on Meteosat Second Generation (MSG) images and generated at the so-called "sea breeze front". This is the limit of the penetration of the sea breeze inland. The sea breeze circulation is a phenomenon that arises when land and sea surface temperatures reveal strong variations. This generates a landward wind that creates a cloud-free area starting from the coast line and ending at the sea breeze front. With the new geostationary meteorological sensors like MSG, this band of cloud-free area can clearly be seen. The automatic analysis of the sea breeze front with such image sensors (instead of using local measurements) is then of great importance. It has the precious advantage to extract huge amount of data and to get rid of the use of local sensors. Unfortunately, from an image processing point of view, this front appears as the limit of a very textured area. It is sometimes disturbed by clouds located in higher layers of the atmosphere. Due to this complexity, conventional detection methods issued from computer vision are not adapted. In this paper we propose an approach that automatically detects fronts in images and we apply this framework to the sea breeze fronts. The methodology is based on the well-known active contour method (or "snake") issued from the computer vision community. The specific textures involved as well as the transparency phenomena are dealt with some properties of the wavelet decomposition of the images. This decomposition enables to compute several criteria related to the presence or not of a front that are combined using the Dempster-Shafer theory. The validation of our approach is done on synthetic and real data. It is important to outline that the presented theoretical framework is not only devoted to the detection of the sea breeze front but can also be used to detect any others textured patterns.
机译:本文涉及卫星图像前沿的检测。我们专注于在Meteosat第二代(MSG)图像上可见并在所谓的“海风锋”处生成的云的某些特定纹理图案。这是海风向内陆渗透的极限。海风循环是陆地和海表温度显示出强烈变化时出现的现象。这会产生陆风,从海岸线开始一直到海风锋结束,形成无云区域。借助像MSG这样的新型地球静止气象传感器,可以清楚地看到这一带无云区域。因此,利用这种图像传感器(而不是使用本地测量值)自动分析海风锋面非常重要。它具有提取大量数据并摆脱使用本地传感器的宝贵优势。不幸的是,从图像处理的角度来看,该正面似乎是非常有纹理的区域的限制。有时它会被位于大气高层的云干扰。由于这种复杂性,因此不适用于由计算机视觉发布的常规检测方法。在本文中,我们提出了一种自动检测图像前沿的方法,并将此框架应用于海风前沿。该方法基于计算机视觉社区发布的众所周知的主动轮廓方法(或“蛇”)。涉及的特定纹理以及透明度现象都通过图像的小波分解的某些特性来处理。通过分解,可以计算与使用Dempster-Shafer理论组合的与前沿的存在与否相关的多个标准。我们的方法的验证是在综合和真实数据上完成的。重要的是概述所提出的理论框架不仅用于检测海风锋线,而且还可以用于检测其他任何纹理图案。

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