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Depth-dependent lag, persistence, and hydro-thermal coupling of soil moisture in a basin of Northern China
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DOI：10.1016/j.jhydrol.2026.136178.png)
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Abstract
En 中文
• Soil moisture shifted from highly variable surface dynamics to stable deep-soil storage. • Vertical coupling weakened and propagation lag increased markedly toward deeper soil. • Soil moisture persistence increased from 14 d at 3 cm to 37 d at 50 cm. • Soil moisture–temperature coupling shifted from negative in shallow soil to positive at depth. • Clay and elevation exerted distinct controls on deep moisture dynamics and hydrothermal coupling.
Keywords:
Soil moisture dynamics
Vertical propagation
Persistence
Soil moisture-temperature coupling
Environmental controls
Shandian River Basin
Journal
IF:
6.3
Papers:
2.3W
Citations:
9.8W
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Cited Papers