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Long-Term Satellite Monitoring of the Slumgullion Landslide Using Space-Borne Synthetic Aperture Radar Sub-Pixel Offset Tracking

机译:利用空射合成孔径雷达子像素偏移跟踪对长谷滑坡进行长期卫星监测

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Kinematic characterization of a landslide at large, small, and detailed scale is today still rare and challenging, especially for long periods, due to the difficulty in implementing demanding ground surveys with adequate spatiotemporal coverage. In this work, the suitability of space-borne synthetic aperture radar sub-pixel offset tracking for the long-term monitoring of the Slumgullion landslide in Colorado (US) is investigated. This landslide is classified as a debris slide and has so far been monitored through ground surveys and, more recently, airborne remote sensing, while satellite images are scarcely exploited. The peculiarity of this landslide is that it is subject to displacements of several meters per year. Therefore, it cannot be monitored with traditional synthetic aperture radar differential interferometry, as this technique has limitations related to the loss of interferometric coherence and to the maximum observable displacement gradient/rate. In order to overcome these limitations, space-borne synthetic aperture radar sub-pixel offset tracking is applied to pairs of images acquired with a time span of one year between August 2011 and August 2013. The obtained results are compared with those available in the literature, both at landslide scale, retrieved through field surveys, and at point scale, using airborne synthetic aperture radar imaging and GPS. The comparison showed full congruence with the past literature. A consistency check covering the full observation period is also implemented to confirm the reliability of the technique, which results in a cheap and effective methodology for the long-term monitoring of large landslide-induced movements.
机译:由于难以实施具有足够的时空覆盖范围的要求苛刻的地面勘测,因此在大,小和详细规模的滑坡运动学表征方面,今天仍然是罕见且具有挑战性的,特别是对于长期而言。在这项工作中,研究了星载合成孔径雷达亚像素偏移跟踪对科罗拉多州(美国)Slumgullion滑坡的长期监测的适用性。该滑坡被归类为泥石流,到目前为止,它已通过地面勘测和最近的机载遥感进行了监测,而很少利用卫星图像。这种滑坡的特殊性在于它每年要承受几米的位移。因此,它不能用传统的合成孔径雷达差分干涉法进行监视,因为该技术具有与干涉相干性损失和最大可观察到的位移梯度/速率有关的限制。为了克服这些限制,将星载合成孔径雷达亚像素偏移跟踪应用于在2011年8月至2013年8月之间的时间跨度为一年的图像对中的获得。将获得的结果与文献中的结果进行比较,既可以通过滑坡进行实地调查,也可以使用机载合成孔径雷达成像和GPS在点规模进行。比较表明与过去的文献完全一致。还进行了覆盖整个观测期的一致性检查,以确认该技术的可靠性,从而为长期监测大型滑坡诱发的运动提供了一种廉价而有效的方法。

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