Mobile QR Code QR CODE : Journal of the Korean Society of Civil Engineers

References

1
Chen, B., Maurer, J., Gong, W. (2025). Applications of UAV in landslide research: a review, Landslides, 22, 3029-3048.DOI
2
Chen, S. C., Chen, C. Y., Huang, W. Y. (2019). Exploring landslide erosion volume-area scaling relationships by slip depth using changes in DTMs for basin sediment volume estimation, Journal of Mountain Science, 16(3), 581-594.DOI
3
Cucchiaro, S., Maset, E., Cavalli, M., Crema, S., Marchi, L., Beinat, A., Cazorzi, F. (2020). How does co-registration affect geomorphic change estimates in multi-temporal surveys?, GIScience & Remote Sensing, 57(5), 611-632.DOI
4
He, H., Ming, Z., Zhang, J., Wang, L., Yang, R., Chen, T., Zhou, F. (2024). Robust estimation of landslide displacement from multitemporal UAV photogrammetry-derived point clouds, IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 17, 6627-6641.DOI
5
Larsen, I. J., Montgomery, D. R., Korup, O. (2010). Landslide erosion controlled by hillslope material, Nature Geoscience, 3, 247-251.DOI
6
Lelli, F., Mulas, M., Critelli, V., Fabbiani, C., Tondo, M., Aleotti, M., Corsini, A. (2025). Leveraging high-frequency UAV–LiDAR surveys to monitor earthflow dynamics—The Baldiola landslide case study, Remote Sensing, 17(15), 2657.DOI
7
Rengers, F. K., McGuire, L. A., Kean, J. W., Staley, D. M., Dobre, M., Robichaud, P. R., Swetnam, T. (2021). Movement of sediment through a burned landscape: Sediment volume observations and model comparisons in the San Gabriel Mountains, California, USA, Journal of Geophysical Research: Earth Surface, 126(7).DOI
8
Schaffrath, K. R., Belmont, P., Wheaton, J. M. (2015). Landscape-scale geomorphic change detection: Quantifying spatially variable uncertainty and circumventing legacy data issues, Geomorphology, 250, 334-348.DOI
9
Wheaton, J. M., Brasington, J., Darby, S. E., Sear, D. A. (2010). Accounting for uncertainty in DEMs from repeat topographic surveys: improved sediment budgets, Earth Surface Processes and Landforms, 35(2), 136-156.DOI