评估无人驾驶航空系统从侵蚀地形采集数据的飞行计划

Valentina Nikolova, Veselina Gospodinova, Asparuh Kamburov
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引用次数: 0

摘要

精确的数据制图和可视化对于检测和监测斜坡形态动力学(包括侵蚀过程)以及研究小型侵蚀地貌(山丘和沟壑)至关重要。当前研究的目的是研究无人机系统(UAS)的飞行几何形状如何影响摄影测量处理产品的准确性,这些产品涉及坡面冲刷和雨水形成的临时小溪造成的小型侵蚀地貌。2021 年 10 月,在一个平均海拔约 650 米的丘陵至低山地区进行了三次不同几何形状的无人机飞行,在那里观察到了侵蚀过程。无人机系统图像处理采用的是结构-运动(SfM)摄影测量法。生成了基于摄影测量的点云、数字地表模型(DSM)和正射影像等高分辨率产品。通过均方根误差 (RMSE)、长度测量、云与云比较以及 DSM 的三维空间 GIS 分析,对获得的数据进行了比较和评估。结果表明,所考虑的摄影测量产品之间的差异很小,这些产品是通过天顶视角和斜视(45°-单条和 60°-交叉条)几何生成的。通过对所获得的摄影测量产品进行复杂分析,60° 交叉条带图像在研究具有缓慢斜坡形态动力学的侵蚀地形方面具有优势。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessment of Unmanned Aerial System Flight Plans for Data Acquisition from Erosional Terrain
Accurate data mapping and visualization are of crucial importance for the detection and monitoring of slope morphodynamics, including erosion processes and studying small erosional landforms (rills and gullies). The purpose of the current research is to examine how the flight geometry of unmanned aerial systems (UASs) could affect the accuracy of photogrammetric processing products, concerning small erosion landforms that are a result of slope wash and temporary small streams formed by rain. In October 2021, three UAS flights with a different geometry were carried out in a hilly to a low-mountain area with an average altitude of about 650 m where erosion processes are observed. UAS imagery processing was carried out using structure-from-motion (SfM) photogrammetry. High-resolution products such as photogrammetric-based point clouds, digital surface models (DSMs) and orthophotos were generated. The obtained data were compared and evaluated by the root mean square error (RMSE), length measurement, cloud-to-cloud comparison, and 3D spatial GIS analysis of DSMs. The results show small differences between the considered photogrammetric products generated by nadir-viewing and oblique-viewing (45°—single strip and 60°—cross strips) geometry. The complex analysis of the obtained photogrammetric products gives an advantage to the 60°—cross strips imagery, in studying erosional terrains with slow slope morphodynamics.
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