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Tree-ring-based moisture variability in western Tianshan Mountains since A.D. 1882 and its possible driving mechanism
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文摘

The consistently dominant climatic factor of tree-ring growth in Tianshan Mountains is verified.

Tree rings provide three century climate records: precipitation, SPEI and PDSI.

Historical change characteristic of moisture since A.D. 1882 is explored.

Possible variability driving mechanism of moisture is revealed.

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