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This study evaluates soil moisture drydown timescales over the Tibetan Plateau using SMAP satellite data and in situ observations from five sensor networks. Findings indicate that SMAP-derived drydown timescales are generally shorter than in situ measurements, with a notable southeast-to-northwest gradient influenced by elevation, soil texture, and vegetation. The research highlights the importance of addressing sensing depth and spatial representativeness for accurate drought diagnostics and understanding

Author

taufikconserve

Language

EN