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Automatic Extraction and Analysis of Ice Layering in Radar Sounder Data

机译:雷达测深仪数据中冰层的自动提取和分析

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Nowadays, the interest on the development of orbiting radar sounders for the observation of Earth polar areas is increasing. In this context, the analysis of the structure of the ice stratigraphy is of primary importance for the study of the past history and for the prediction of the evolution of icy environments. However, as proven by planetary missions, orbiting radar sounders provide a huge amount of data. Thus, the development of automatic techniques for the analysis of these data is of fundamental importance for proper data exploitation. In this paper, we propose a novel method for the automatic detection of subsurface linear features from radar sounder data acquired in icy regions showing extended layering. The proposed method allows the estimation of the position of the linear features with subpixel accuracy. Moreover, each detected linear interface is treated as a single object which is completely described by the position of its points, the estimated local width, and the contrast. This allows the direct measurement of geometrical and radiometric parameters (e.g., slope angle and intensity) without the need of further postprocessing steps. This paper also proposes some measurements for deriving from the output of the proposed technique important variables that can characterize quantitatively the properties of the detected linear features (e.g., mean depth and mean intensity) and their distribution (e.g., number and density of layers). The effectiveness of the proposed method is confirmed by the results obtained on several radargrams acquired by the Shallow Radar on the North Pole of Mars.
机译:如今,人们对发展用于观测地球极地的轨道雷达测深仪的兴趣与日俱增。在这种情况下,对冰地层结构的分析对于研究过去的历史以及预测冰冷环境的演变至关重要。但是,正如行星飞行任务所证明的那样,绕行雷达探测仪可提供大量数据。因此,开发用于分析这些数据的自动技术对于正确地利用数据至关重要。在本文中,我们提出了一种新的方法,该方法可从在冰层区域显示扩展分层的雷达测深仪数据自动检测地下线性特征。所提出的方法允许以亚像素精度估计线性特征的位置。此外,每个检测到的线性界面都被视为一个单独的对象,该对象完全由其点的位置,估计的局部宽度和对比度来描述。这允许直接测量几何和辐射测量参数(例如,倾斜角和强度),而无需进一步的后处理步骤。本文还提出了一些测量方法,可以从所提出的技术的输出中得出重要的变量,这些变量可以定量地表征检测到的线性特征的特性(例如平均深度和平均强度)及其分布(例如层的数量和密度)。该方法的有效性通过火星北极浅层雷达获得的若干雷达图的结果得到证实。

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