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Algorithm evaluation demonstrates high-accuracy permafrost thaw slump detection in satellite imagery, suggesting viable automated offline polar terrain mapping.
Climate warming is accelerating Arctic permafrost degradation and intensifying retrogressive thaw slump (RTS) activity. To address the limited availability of RTS samples, large target-scale variation and unstable bounding-box localization in complex high-resolution optical remote-sensing imagery, this study proposes an improved DINO-based detection framework, SM-DINO. The framework uses cross-architecture feature-level knowledge distillation to transfer high-level semantic information from a ViT-S/16 teacher model pre-trained on a large remote-sensing data set to a ResNet-50 backbone. It further introduces a multi-scale dilated feature aggregation (MDFA) module and a geometry-modulated focal IoU (GMF-IoU) loss. Experiments on a high-resolution RGB imagery data set from Banks Island, Canada, show that SM-DINO achieves an mAP0.5:0.95 of 86.6% and mAP0.5 of 98.0%. These values are modestly higher than those of the original DINO baseline. The results suggest that remote-sensing knowledge transfer, multi-scale feature modelling and geometry-aware regression optimization can support RTS candidate-target detection in complex polar environments, while the method remains most suitable for server-side offline mapping rather than real-time deployment.
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Hou et al. (2026) studied this question.
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