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Factors Influencing the Accuracy of Shallow Snow Depth Measured Using UAV-Based Photogrammetry

Authors
Lee, SangkuPark, JeonghaChoi, EunsooKim, Dongkyun
Issue Date
Feb-2021
Publisher
MDPI
Keywords
snow; photogrammetry; UAV; ground control points; drone; multi-temporal
Citation
REMOTE SENSING, v.13, no.4, pp.1 - 20
Journal Title
REMOTE SENSING
Volume
13
Number
4
Start Page
1
End Page
20
URI
https://scholarworks.bwise.kr/hongik/handle/2020.sw.hongik/15615
DOI
10.3390/rs13040828
ISSN
2072-4292
Abstract
Factors influencing the accuracy of UAV-photogrammetry-based snow depth distribution maps were investigated. First, UAV-based surveys were performed on the 0.04 km(2) snow-covered study site in South Korea for 37 times over the period of 13 days under 16 prescribed conditions composed of various photographing times, flight altitudes, and photograph overlap ratios. Then, multi-temporal Digital Surface Models (DSMs) of the study area covered with shallow snow were obtained using digital photogrammetric techniques. Next, the multi-temporal snow depth distribution maps were created by subtracting the snow-free DSM from the multi-temporal DSMs of the study area. Then, snow depth in these UAV-Photogrammetry-based snow maps were compared to the in situ measurements at 21 locations. The accuracy of each of the multi-temporal snow maps were quantified in terms of bias (median of residuals, Q Delta D) and precision (the Normalized Median Absolute Deviation, NMAD). Lastly, various factors influencing these performance metrics were investigated. The results are as follows: (1) the Q Delta D and NMAD of the eight surveys performed at the optimal condition (50 m flight altitude and 80% overlap ratio) ranged from -2.30 cm to 5.90 cm and from 1.78 cm to 4.89 cm, respectively. The best survey case had -2.30 cm of Q Delta D and 1.78 cm of NMAD; (2) Lower UAV flight altitude and greater photograph overlap lower the NMAD and Q Delta D; (3) Greater number of Ground Control Points (GCPs) lowers the NMAD and Q Delta D; (4) Spatial configuration and accuracy of GCP coordinates influenced the accuracy of the snow depth distribution map; (5) Greater number of tie-points leads to higher accuracy; (6) Smooth fresh snow cover did not provide many tie-points, either resulting in a significant error or making the entire photogrammetry process impossible.
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