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Minute-scale observations reveal hydrothermal coupling dynamics of soil freeze–thaw processes in the alpine source region of the Yellow River
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DOI：10.1016/j.catena.2026.110490.png)
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Abstract
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• Minute-scale observations reveal five freeze–thaw stages and hydrothermal transitions. • The freeze–thaw front's 0 °C crossing lag increases with depth. • The temperature–unfrozen water content relation follows a power-law. • Freeze–thaw deformation concentrates near the surface and decays rapidly with depth.
Keywords:
Climate warming
Permafrost degradation
Hydro–thermal coupling
The Yellow River
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