Landslides represent hazardous phenomena, often with significant implications. Monitoring landslides with time‐series surface observations can indicate surface failure. Unmanned aerial vehicles (UAVs) employing compact digital cameras, in conjunction with structure‐from‐motion (SfM) and multi‐view stereo (MVS) image processing approaches, have become commonplace in the geoscience research community. These methods offer relatively low‐cost, flexible solutions for many geomorphological monitoring applications. However, conventionally ground control points (GCPs) are required for registration purposes, the provision of which is often expensive, difficult or even impracticable in hazardous and inaccessible terrain.
In an attempt to overcome the reliance on GCPs, this paper reports research that has developed a morphology‐based strategy to co‐register multi‐temporal UAV‐derived products. It applies the attribute of curvature in combination with the scale‐invariant feature transform algorithm, to generate time‐invariant curvature features, which serve as pseudo‐GCPs. Openness, a surface morphological digital elevation model derivative, is applied to identify relatively stable ground regions from which pseudo‐GCPs are selected. A sensitivity threshold quantifies the minimum detectable change alongside unresolved biases and misalignment errors. The approach is evaluated at two study sites in the UK, first at Sandford with artificially induced surface change, and second at an active landslide at Hollin Hill, with multi‐epoch SfM‐MVS products derived from a consumer‐grade UAV. Elevation changes and annual displacement rates at dm‐level are estimated, with optimal results achieved over winter periods. The morphology‐based co‐registration strategy resulted in relative error ratios (i.e. mean error divided by average flying height) in the range 1:800–2500, comparable with those reported by similar studies conducted with UAVs augmented with real time kinematic (RTK)‐Global Navigation Satellite Systems. Analysis demonstrates the potential of the morphology‐based strategy for a semi‐automatic, and practical co‐registration approach to quantify surface motion. This can ultimately complement geotechnical and geophysical investigations and support the understanding of landslide behaviour, model prediction and construction of measures for mitigating risks. © 2018 John Wiley & Sons, Ltd.