Reconstruction of biological drought conditions during the past 2847 years in an alpine environment of the northeastern Tibetan Plateau, China, and possible linkages to solar forcing
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文摘

An in situ biological drought index was developed using water-balance modeling and geographic information systems.

Drought history of northeastern Tibetan Plateau was reconstructed back to 843 BCE based on a tree-ring chronology.

Drought variability in northeastern Tibetan Plateau was closely related to the 210-year de Vries solar cycle since 1300 CE.

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