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Soil moisture drove vegetation change on the Qinghai-Tibetan Plateau
Soil moisture constraints override atmospheric aridity in governing vegetation dynamics across the warming Qinghai-Tibetan Plateau, with regional variation depending on basin hydrogeography.
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Modified isotope model estimates higher advected moisture fraction
Modified isotopic mixing model for estimating precipitation moisture sources in southwest China using transpiration ratios and leaf area index constraints.
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Freeze–thaw reshapes water, salt, and heat in saline farmland soil
Freeze-thaw driven water-salt redistribution in saline farmland soils: quantified hydrothermal parameters and coupled migration mechanisms from field-laboratory verification.
