The role of permafrost and soil water in distribution of alpine grassland and its NDVI dynamics on the Qinghai-Tibetan Plateau
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文摘
The NDVI trend and distribution of alpine grassland at plateau scale were studied. They were analyzed in relation to permafrost, soil moisture and LST-NDVI. Permafrost and soil moisture were important for grassland distribution and change. The LST-NDVI relationship only explained < 50% variation of vegetation changing trend. Other factors may overwhelm hydro-thermal conditions in affecting vegetation growth.

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