| Abstract: |
Accurate snow depth mapping in mountain terrain remains challenging because snow distribution is strongly controlled by wind exposure, slope configuration, surface roughness, and microtopographic complexity. These controls are especially important on rock glaciers, where ridges, furrows, depressions, steep fronts, and coarse blocky surfaces create strong small-scale variability in snow deposition, redistribution, and retention. In such environments, snow cover patterns depend not only on seasonal snowfall amount, but also on the interaction between local terrain morphology and snow-transport processes. This study presents a multi-temporal UAV photogrammetry workflow for monitoring snow depth over the Galeșu Rock Glacier, Retezat Mountains, Romania, based on repeated surveys acquired between 2023 and 2026. Multiple winter campaigns, mainly conducted in February and March, were processed using Structure-from-Motion techniques to generate high-resolution orthomosaics and digital surface models of snow-covered terrain. Snow depth was derived by differencing these models against a snow-free reference surface, enabling detailed mapping of snow distribution and its seasonal evolution across the rock glacier. The workflow was further designed to investigate how terrain morphology controls snow accumulation patterns. UAV-derived snow depth maps were coupled with morphometric analysis based on terrain metrics including slope, aspect, curvature, roughness, and topographic position. Particular attention was given to the influence of characteristic rock glacier microforms, especially furrows and ridges, on preferential snow deposition and storage. These elements act as local traps or exposed zones, generating marked contrasts in snow accumulation through wind redistribution and differential melt. Preliminary results from the first two surveys in 2023 reveal pronounced snow-depth heterogeneity, with values ranging from 0 m to over 3 m across significant portions of the landform, together with a clear increase in snow accumulation from winter to spring. Areas characterized by sheltered depressions, higher roughness, and negative topographic position generally retain deeper and more persistent snow, whereas exposed ridges and convex surfaces show reduced accumulation. In addition, this study also presents the UAV surveys acquired in 2024, 2025, and 2026, providing a multi-year perspective on snow deposition and accumulation under contrasting winter conditions. The UAV-based analysis is further complemented by correlation with a time-lapse camera installed on site, which offers continuous visual monitoring of snow deposition, persistence, and melt evolution throughout the snow season. This integration helps link discrete UAV surveys with the temporal dynamics of snow cover development and disappearance. Initial validation against in situ measurements indicated mean errors of -0.24 m in winter and -0.14 m in spring, with the highest accuracy observed over vegetation-free surfaces unaffected by canopy-related elevation bias. Statistical comparison between furrows and ridges demonstrates a clear microtopographic signal, with mean snow-depth differences of about 1.2-1.5 m between these landform types. Overall, the new results highlight the value of UAV-SfM photogrammetry for repeated snow monitoring in complex periglacial terrain and support its integration with terrain morphometry for high-resolution analysis of snow-topography interactions. |