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Automatic polar ice thickness estimation from SAR imagery

机译:SAR图像自动极性冰厚度估计

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Global warming has caused serious damage to our environment in recent years. Accelerated loss of ice from Greenland and Antarctica has been observed in recent decades. The melting of polar ice sheets and mountain glaciers has a considerable influence on sea level rise and altering ocean currents, potentially leading to the flooding of the coastal regions and putting millions of people around the world at risk. Synthetic aperture radar (SAR) systems are able to provide relevant information about subsurface structure of polar ice sheets. Manual layer identification is prohibitively tedious and expensive and is not practical for regular, long-term ice-sheet monitoring. Automatic layer finding in noisy radar images is quite challenging due to huge amount of noise, limited resolution and variations in ice layers and bedrock. Here we propose an approach which automatically detects ice surface and bedrock boundaries using distance regularized level set evolution. In this approach the complex topology of ice and bedrock boundary layers can be detected simultaneously by evolving an initial curve in radar imagery. Using a distance regularized term, the regularity of the level set function is intrinsically maintained that solves the reinitialization issues arising from conventional level set approaches. The results are evaluated on a large dataset of airborne radar imagery collected during IceBridge mission over Antarctica and Greenland and show promising results in respect to hand-labeled ground truth.
机译:近年来,全球变暖对我们的环境造成严重损害。近几十年来观察到格陵兰岛和南极洲的加速失去冰。极地冰盖和山地冰川的熔化对海平面上升和改变海洋电流具有相当大的影响,可能导致沿海地区的洪水,并将全世界数百万人口造成风险。合成孔径雷达(SAR)系统能够提供有关极地冰盖的地下结构的相关信息。手动层识别非常繁琐,昂贵且不实用,对于常规,长期的冰盖监测。由于噪音,分辨率有限,冰层和基岩的变化,自动层在嘈杂的雷达图像中发现非常具有挑战性。在这里,我们提出了一种方法,使用距离正则水平集进化自动检测冰面和基岩边界。在这种方法中,通过在雷达图像中演化初始曲线,可以同时检测冰和基岩边界层的复杂拓扑。使用距离正规术语,本质上维护级别集功能的规律性,解决了传统水平集方法所产生的重新初始化问题。结果在南极洲和格陵兰岛的Icebridge Mission期间收集的机载雷达图像的大型数据集进行了评估,并表现出对手工标记的原始事实的有希望的结果。

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