Accuracy of snow depth estimation in mountain and prairie environments by an unmanned aerial vehicle

• Published in: The cryosphere Vol. 10; no. 6; pp. 2559 - 2571
• Main Authors: Harder, Phillip, Schirmer, Michael, Pomeroy, John, Helgason, Warren
• Format: Journal Article
• Language: English
• Published: Katlenburg-Lindau Copernicus GmbH 02-11-2016; Copernicus Publications
• Subjects: Accuracy; Airborne lasers; Airborne remote sensing; Airborne sensing; Aircraft; Algorithms; Analysis; Atmospheric models; Automation; Cryosphere; Depletion; Depth; Digital cameras; Earth science; Global positioning systems; GPS; Imagery; Lasers; Miniature aircraft; Motion perception; Mountains; Photogrammetry; Photography; Plant cover; Prairies; Predation; Remote sensing; Remotely piloted vehicles; Sensors; Signal to noise ratio; Snow; Snow accumulation; Snow cover; Snow depth; Snowpack; Spatial distribution; Spatial variability; Spatial variations; Stubble; Surface properties; Temporal variations; Unmanned aerial vehicles; Vegetation; Vegetation cover; Water resources; Weather forecasting; Wind; Wind speed; Canada; Saskatchewan Canada
• ISSN: 1994-0424; 1994-0416; 1994-0424; 1994-0416
• DOI: 10.5194/tc-10-2559-2016

Quantifying the spatial distribution of snow is crucial to predict and assess its water resource potential and understand land–atmosphere interactions. High-resolution remote sensing of snow depth has been limited to terrestrial and airborne laser scanning and more recently with application of structure from motion (SfM) techniques to airborne (manned and unmanned) imagery. In this study, photography from a small unmanned aerial vehicle (UAV) was used to generate digital surface models (DSMs) and orthomosaics for snow cover at a cultivated agricultural Canadian prairie and a sparsely vegetated Rocky Mountain alpine ridgetop site using SfM. The accuracy and repeatability of this method to quantify snow depth, changes in depth and its spatial variability was assessed for different terrain types over time. Root mean square errors in snow depth estimation from differencing snow-covered and non-snow-covered DSMs were 8.8 cm for a short prairie grain stubble surface, 13.7 cm for a tall prairie grain stubble surface and 8.5 cm for an alpine mountain surface. This technique provided useful information on maximum snow accumulation and snow-covered area depletion at all sites, while temporal changes in snow depth could also be quantified at the alpine site due to the deeper snowpack and consequent higher signal-to-noise ratio. The application of SfM to UAV photographs returns meaningful information in areas with mean snow depth  >  30 cm, but the direct observation of snow depth depletion of shallow snowpacks with this method is not feasible. Accuracy varied with surface characteristics, sunlight and wind speed during the flight, with the most consistent performance found for wind speeds  < 10 m s−1, clear skies, high sun angles and surfaces with negligible vegetation cover.