In the last decade advances in surveying technology have opened up the possibility of representing topography and monitoring surface changes over experimental plots (<10 m2) in high resolution (~103 points m-1). Yet the representativeness of these small plots is limited. With ‘Structure-from-Motion’ (SfM) and ‘Multi-View Stereo’ (MVS) techniques now becoming part of the geomorphologist's toolkit, there is potential to expand further the scale at which we characterise topography and monitor geomorphic change morphometrically. Moving beyond previous plot-scale work using Terrestrial Laser Scanning (TLS) surveys, this paper validates robustly a number of SfM-MVS surveys against total station and extensive TLS data at three nested scales: plots...
High-resolution Digital Elevation Models (DEMs) have proven to be very useful when analyzing geomorp...
High-resolution digital elevation models (DEMs) are useful for the detailed mapping of geomorphologi...
Soil erosion is a decisive earth surface process strongly influencing the fertility of arable land. ...
In the last decade advances in surveying technology have opened up the possibility of representing t...
Structure-from-motion (SfM) photogrammetry from unmanned aerial system (UAS) imagery is an emerging ...
Erosion and deposition processes in badland areas are usually estimated using traditional observatio...
Soil erosion is a complex geomorphological process with varying influences of different impacts at d...
In this paper, three methods (Terrestrial Laser Scanner (TLS), terrestrial Structure from Motion pho...
Quantifying the extent of soil erosion at a fine spatial resolution can be time consuming and costly...
International audienceSurveying techniques such as terrestrial laser scanner have recently been used...
Soil erosion is a major threat to soil fertility, food security and water resources. Besides a quant...
Erosion and deposition processes in badland areas are usually estimated using traditional observatio...
The Catterline Bay, located in North East Scotland, is prone to erosion processes. Using Terrestrial...
Airborne laser scanning (ALS) and terrestrial laser scanning (TLS) technologies capture spatially de...
Quantifying the extent of soil erosion at a fine spatial resolution can be time consuming and costly...
High-resolution Digital Elevation Models (DEMs) have proven to be very useful when analyzing geomorp...
High-resolution digital elevation models (DEMs) are useful for the detailed mapping of geomorphologi...
Soil erosion is a decisive earth surface process strongly influencing the fertility of arable land. ...
In the last decade advances in surveying technology have opened up the possibility of representing t...
Structure-from-motion (SfM) photogrammetry from unmanned aerial system (UAS) imagery is an emerging ...
Erosion and deposition processes in badland areas are usually estimated using traditional observatio...
Soil erosion is a complex geomorphological process with varying influences of different impacts at d...
In this paper, three methods (Terrestrial Laser Scanner (TLS), terrestrial Structure from Motion pho...
Quantifying the extent of soil erosion at a fine spatial resolution can be time consuming and costly...
International audienceSurveying techniques such as terrestrial laser scanner have recently been used...
Soil erosion is a major threat to soil fertility, food security and water resources. Besides a quant...
Erosion and deposition processes in badland areas are usually estimated using traditional observatio...
The Catterline Bay, located in North East Scotland, is prone to erosion processes. Using Terrestrial...
Airborne laser scanning (ALS) and terrestrial laser scanning (TLS) technologies capture spatially de...
Quantifying the extent of soil erosion at a fine spatial resolution can be time consuming and costly...
High-resolution Digital Elevation Models (DEMs) have proven to be very useful when analyzing geomorp...
High-resolution digital elevation models (DEMs) are useful for the detailed mapping of geomorphologi...
Soil erosion is a decisive earth surface process strongly influencing the fertility of arable land. ...