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Monitoring mass movements using georeferenced time-lapse photography: Ritigraben rock glacier, western Swiss Alps

机译:使用经过地理定位的延时摄影来监测群众运动:瑞士西部阿尔卑斯山的里蒂格拉本岩石冰川

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摘要

An automatic method was developed to monitor rock glacier kinematics. Displacements derived from monoscopic time-lapse images were scaled and projected into the Swiss Coordinate System CH1903. We tested this method at the front of the rapidly creeping Ritigraben rock glacier, where time-lapse pictures of the rock glacier front were taken by an automatic camera with a temporal resolution of 3 h. The images were automatically processed using a Matlab algorithm. The output data were spatially resolved creep velocities between successive images and mean relative velocities over time. The digital elevation model used for the projection of the time-lapse data was acquired using terrestrial laser scanning (TLS). The resulting horizontal displacement velocities and accelerations were validated against GPS data measured at one point on the rock glacier front. The high temporal resolution of the time-lapse image velocities provided new insights on the kinematics of the rock glacier front, which could not have been discerned with the GPS or TLS measurements applied. The Ritigraben study site is particularly suitable for our approach due to the temporally constant movement directions. Snow coverage and fog are disturbing factors which can lead to failure of the method.
机译:开发了一种自动方法来监测岩石冰川运动学。从单眼延时图像得出的位移被缩放并投影到瑞士坐标系CH1903中。我们在快速蠕动的Ritigraben岩石冰川的前部测试了该方法,该岩石冰川前部的延时照片是用时间分辨率为3 h的自动照相机拍摄的。使用Matlab算法自动处理图像。输出数据是连续图像之间的空间分辨蠕变速度以及随时间的平均相对速度。使用地面激光扫描(TLS)获取了用于投影延时数据的数字高程模型。相对于在冰川冰河前缘某一点测得的GPS数据验证了产生的水平位移速度和加速度。时移图像速度的高时间分辨率为岩石冰川前缘的运动学提供了新的见识,而应用GPS或TLS测量无法发现这一点。 Ritigraben研究站点由于时间上恒定的移动方向而特别适合我们的方法。积雪和雾是干扰因素,可能导致方法失败。

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  • 来源
    《Cold regions science and technology》 |2018年第1期|127-134|共8页
  • 作者单位

    WSL Inst Snow & Avalanche Res SLF, Davos, Switzerland;

    WSL Inst Snow & Avalanche Res SLF, Davos, Switzerland;

    Swiss Fed Inst Technol, Inst Geodesy & Photogrammetry, Zurich, Switzerland;

    Swiss Fed Inst Technol, Comp Engn & Networks Lab, Zurich, Switzerland;

    WSL Inst Snow & Avalanche Res SLF, Davos, Switzerland;

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