Co-variability of the summer NDVIs on the eastern Tibetan Plateau and in the Lake Baikal region: Associated climate factors and atmospheric circulation.

The normalized NDVI over the eastern Tibetan Plateau shows a decreasing trend of –0.33/decade (significant at the 90% confidence level), whereas the normalized NDVI over the central and western Tibetan Plateau generally shows an increasing trend (figure omitted).

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There was also an increasing trend in precipitation over the Tibetan Plateau [ 14 , 15 ].

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