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UAV photogrammetry and structure from motion to assess calving dynamics at Store Glacier, a large outlet draining the Greenland ice sheet

机译:无人机摄影测量和结构从运动到评估Store Glacier的产犊动态,Store Glacier是排泄格陵兰冰原的大型出口

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摘要

This study presents the application of a cost-effective, unmanned aerial vehicle (UAV) to investigate calving dynamics at a major marine-terminating outlet glacier draining the western sector of the Greenland ice sheet. The UAV was flown over Store Glacier on three sorties during summer 2013 and acquired over 2000 overlapping, geo-tagged images of the calving front at an ?40 cm ground sampling distance. Stereo-photogrammetry applied to these images enabled the extraction of high-resolution digital elevation models (DEMs) with vertical accuracies of ?1.9m which were used to quantify glaciological processes from early July to late August 2013. The central zone of the calving front advanced by ?500 m, whilst the lateral margins remained stable. The orientation of crevasses and the surface velocity field derived from feature tracking indicates that lateral drag is the primary resistive force and that ice flow varies across the calving front from 2.5md-1 at the margins to in excess of 16md-1 at the centreline. Ice flux through the calving front is 3.8?107 m3 d-1, equivalent to 13.9 Gt a-1 and comparable to flux-gate estimates of Store Glacier's annual discharge. Water-filled crevasses were present throughout the observation period but covered a limited area of between 0.025 and 0.24% of the terminus and did not appear to exert any significant control over fracture or calving. We conclude that the use of repeat UAV surveys coupled with the processing techniques outlined in this paper have great potential for elucidating the complex frontal dynamics that characterise large calving outlet glaciers.
机译:这项研究提出了一种具有成本效益的无人驾驶飞机(UAV)的应用,以调查在排泄格陵兰冰原西部区域的主要海洋终端出口冰川的产犊动力学。该无人机于2013年夏季分三架次在Store Glacier上空飞行,并在距地面40厘米的距离上采集了2000多张重叠的,带有地理标签的产犊前锋图像。将立体摄影测量技术应用于这些图像,可以提取垂直精度为1.9m的高分辨率数字高程模型(DEM),这些模型用于量化2013年7月初至8月下旬的冰川过程。大约500 m,而侧向边缘保持稳定。裂缝的方向和从特征跟踪得出的表面速度场表明,横向阻力是主要的阻力,并且冰流在整个产犊锋线处从边缘的2.5md-1变化到中心线的16md-1以上。通过产犊前沿的冰通量为3.8?107 m3 d-1,相当于13.9 Gt a-1,可与Store Glacier年排放量的通量闸估算相媲美。在整个观察期内都充满了水的裂缝,但其覆盖范围仅在末端的0.025%至0.24%之间,似乎对骨折或产犊没有任何明显的控制作用。我们得出的结论是,重复进行的无人机调查与本文概述的处理技术的结合,对于阐明大型产犊冰川特征的复杂的前缘动力学具有巨大的潜力。

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