Remote sensing analysis reveals localized soil erosion rates up to 30 mm/year in tropical drylands, highlighting severe degradation hotspots masked by landscape-scale averages.
Quantifying soil erosion in vulnerable tropical drylands is critical for desertification management but remains methodologically challenging due to the spatial limitations of field-based methods. This study introduces a novel framework integrating Small Baseline Subset Interferometric Synthetic Aperture Radar (SBAS-InSAR) with unsupervised statistical clustering to quantify erosion rates and validate spatial heterogeneity in the La Tatacoa dry forest, Colombia. Using 123 Sentinel-1 radar images (from 2018 to 2023), we generated high-resolution displacement velocity maps, which were then integrated with Normalized Difference Vegetation Index (NDVI) data from Sentinel-2 and geomorphometric attributes derived from the ALOS PALSAR Digital Elevation Model. Study-wide mean erosion rates ranged from 0.43 to 0.54 mm/year; however, these averages masked significant localized instability. Time-series K-means clustering of 100 randomized sampling points identified four distinct deformation regimes, statistically confirming that high-velocity zones are structural realities rather than measurement noise. Specifically, Cluster 4 identified critical hotspots where erosion rates reached 30 mm/year exceeding the United States Department of Agriculture (USDA) soil tolerance threshold (0.93 mm/year) by a factor of 32. These hotspots are systematically confined to dissected terrain with slopes > 9 ° and NDVI < 0.15 . By rigorously distinguishing genuine deformation regimes from background variability, this framework provides a scalable, evidence-based tool for prioritizing conservation interventions in data-limited dryland ecosystems.
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Sánchez-Ospina et al. (2026) studied this question.
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