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Tracking rapid permafrost thaw through time
The research demonstrates that site-specific CNN models can effectively detect retrogressive thaw slumps (RTS) using Sentinel-2 satellite data, achieving precision, recall, and F1 values above 0.8. While this approach enables the creation of time series data to approximate greenhouse gas emissions from rapid permafrost thaw, current results show no clear trends due to the 10 m resolution of the satellite data and a lack of diverse validated training data.
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Document type: Research paper
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