首页> 外文期刊>International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences >ANOMALY DETECTION PERFORMANCE COMPARISON ON ANOMALY-DETECTION BASED CHANGE DETECTION ON MARTIAN IMAGE PAIRS
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ANOMALY DETECTION PERFORMANCE COMPARISON ON ANOMALY-DETECTION BASED CHANGE DETECTION ON MARTIAN IMAGE PAIRS

机译:基于异常检测的马氏图像对变化检测的异常检测性能比较

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The surface of Mars has been imaged in visible wavelengths for more than 40 years since the first flyby image taken by Mariner 4 in 1964. With higher resolution from orbit from MOC-NA, HRSC, CTX, THEMIS, and HiRISE, changes can now be observed on high-resolution images from different instruments, including spiders (Piqueux et al., 2003) near the south pole and Recurring Slope Lineae (McEwen et al., 2011) observable in HiRISE resolution. With the huge amount of data and the small number of datasets available on Martian changes, semi-automatic or automatic methods are preferred to help narrow down surface change candidates over a large area.To detect changes automatically in Martian images, we propose a method based on a denoising autoencoder to map the first Martian image to the second Martian image. Both images have been automatically coregistered and orthorectified using ACRO (Autocoregistration and Orthorectification) (Sidiropoulos and Muller, 2018) to the same base image, HRSC (High-Resolution Stereo Camera) (Neukum and Jaumann, 2004; Putri et al., 2018) and CTX (Context Camera) (Tao et al., 2018) orthorectified using their DTMs (Digital Terrain Models) to reduce the number of false positives caused by the difference in instruments and viewing conditions. Subtraction of the codes of the images are then inputted to an anomaly detector to look for change candidates. We compare different anomaly detection methods in our change detection pipeline: OneClassSVM, Isolation Forest, and, Gaussian Mixture Models in known areas of changes such as Nicholson Crater (dark slope streak), using image pairs from the same and different instruments.
机译:自1964年Mariner 4拍摄第一张飞越图像以来,火星表面已经在可见波长下成像了40多年。由于MOC-NA,HRSC,CTX,THEMIS和HiRISE的轨道具有更高的分辨率,现在可以改变在不同仪器的高分辨率图像上观测到的图像,包括在南极附近的蜘蛛(Piqueux等,2003)和在HiRISE分辨率下可观测到的重复斜坡线状体(McEwen等,2011)。由于火星变化的数据量大且数据集数量少,因此首选半自动或自动方法来帮助缩小大范围内的表面变化候选对象。为了在火星图像中自动检测变化,我们提出了一种基于在去噪自动编码器上将第一个火星图像映射到第二个火星图像。两种图像都已使用ACRO(自动变位和正射)(Sidiropoulos和Muller,2018)自动共配准并进行了正射矫正,并将其与同一基本图像HRSC(高分辨率立体相机)(Neukum和Jaumann,2004; Putri等人,2018)结合在一起。和CTX(情境相机)(Tao等人,2018)使用其DTM(数字地形模型)进行了正交矫正,以减少由于仪器和观看条件的差异而导致的误报次数。然后,将图像的代码的减法输入到异常检测器以寻找变化候选者。我们在变化检测管道中比较了不同的异常检测方法:使用来自相同和不同仪器的图像对,在已知变化区域(如Nicholson Crater(暗斜条纹))中使用了OneClassSVM,隔离林和高斯混合模型。

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