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Application of Low-Cost UASs and Digital Photogrammetry for High-Resolution Snow Depth Mapping in the Arctic

机译:低成本无人机和数字摄影测量在北极地区高分辨率雪深测绘中的应用

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摘要

The repeat acquisition of high-resolution snow depth measurements has important research and civil applications in the Arctic. Currently the surveying methods for capturing the high spatial and temporal variability of the snowpack are expensive, in particular for small areal extents. An alternative methodology based on Unmanned Aerial Systems (UASs) and digital photogrammetry was tested over varying surveying conditions in the Arctic employing two diverse and low-cost UAS-camera combinations (500 and 1700 USD, respectively). Six areas, two in Svalbard and four in Greenland, were mapped covering from 1386 to 38,410 m. The sites presented diverse snow surface types, underlying topography and light conditions in order to test the method under potentially limiting conditions. The resulting snow depth maps achieved spatial resolutions between 0.06 and 0.09 m. The average difference between UAS-estimated and measured snow depth, checked with conventional snow probing, ranged from 0.015 to 0.16 m. The impact of image pre-processing was explored, improving point cloud density and accuracy for different image qualities and snow/light conditions. Our UAS photogrammetry results are expected to be scalable to larger areal extents. While further validation is needed, with the inclusion of extra validation points, the study showcases the potential of this cost-effective methodology for high-resolution monitoring of snow dynamics in the Arctic and beyond.
机译:重复获取高分辨率雪深测量值在北极地区具有重要的研究和民用应用。当前,用于捕获积雪的高空间和时间变化的测量方法是昂贵的,特别是对于小面积范围而言。在北极不同的调查条件下,采用两种不同且低成本的UAS相机组合(分别为500和1700美元)对基于无人航空系统(UAS)和数字摄影测量的替代方法进行了测试。绘制了六个区域,其中两个在斯瓦尔巴群岛,四个在格陵兰岛,覆盖了1386至38,410 m的区域。这些地点展示了各种雪面类型,潜在的地形和光照条件,以便在可能受到限制的条件下测试该方法。产生的积雪深度图实现了0.06至0.09 m的空间分辨率。用传统的测雪技术检查后,UAS估计的和测得的积雪深度之间的平均差为0.015至0.16 m。探索了图像预处理的影响,针对不同的图像质量和雪/光条件提高了点云密度和准确性。我们的UAS摄影测量结果有望在更大的范围内扩展。尽管还需要进一步的验证,并包括额外的验证点,但研究表明,这种具有成本效益的方法可用于高分辨率监测北极及其他地区的积雪动力学。

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