Monitoring snow depth change across a range of landscapes with ephemeral snowpacks using structure from motion applied to lightweight unmanned aerial vehicle videos

被引:24
作者
Fernandes, Richard [1 ]
Prevost, Christian [1 ]
Canisius, Francis [1 ]
Leblanc, Sylvain G. [1 ]
Maloley, Matt [1 ]
Oakes, Sarah [1 ]
Holman, Kiyomi [2 ]
Knudby, Anders [2 ]
机构
[1] Nat Resources Canada, Canada Ctr Remote Sensing, Ottawa, ON K1A 0Y7, Canada
[2] Univ Ottawa, Dept Geog Environm & Geomat, Ottawa, ON K1N 6Y5, Canada
关键词
WATER EQUIVALENT; ALPINE TERRAIN; RECONSTRUCTION; MOUNTAIN; FORESTS; UAS;
D O I
10.5194/tc-12-3535-2018
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Differencing of digital surface models derived from structure from motion (SfM) processing of airborne imagery has been used to produce snow depth (SD) maps with between similar to 2 and similar to 15 cm horizontal resolution and accuracies of +/- 10 cm over relatively flat surfaces with little or no vegetation and over alpine regions. This study builds on these findings by testing two hypotheses across a broader range of conditions: (i) that the vertical accuracy of SfM processing of imagery acquired by commercial low-cost unmanned aerial vehicle (UAV) systems can be adequately modelled using conventional photogrammetric theory and (ii) that SD change can be more accurately estimated by differencing snow-covered elevation surfaces rather than differencing a snow-covered and snow-free surface. A total of 71 UAV missions were flown over five sites, ranging from short grass to a regenerating forest, with ephemeral snowpacks. Point cloud geolocation performance agreed with photogrammetric theory that predicts uncertainty is proportional to UAV altitude and linearly related to horizontal uncertainty. The root-mean-square difference (RMSD) over the observation period, in comparison to the average of in situ measurements along similar to 50 m transects, ranged from 1.58 to 10.56 cm for weekly SD and from 2.54 to 8.68 cm for weekly SD change. RMSD was not related to microtopography as quantified by the snow-free surface roughness. SD change uncertainty was unrelated to vegetation cover but was dominated by outliers corresponding to rapid in situ melt or onset; the median absolute difference of SD change ranged from 0.65 to 2.71 cm. These results indicate that the accuracy of UAV-based estimates of weekly snow depth change was, excepting conditions with deep fresh snow, substantially better than for snow depth and was comparable to in situ methods.
引用
收藏
页码:3535 / 3550
页数:16
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