Spatiotemporal dynamic of subtropical forest carbon storage and its resistance and resilience to drought in China.

According to the spatial variation trends in drought ( Figure 3B ), SPEI 12 showed a decreasing trend in 62.13% of the region, with an overall decrease of 0.036(10 a) -1 .

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Spatial analysis showed a clear trend of drought in the subtropical southwest, especially in the Sichuan Basin, which is consistent with previous research findings ( Li et al., 2012 ).

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The results show that: 1) from 1952 to 2019, the interannual drought in subtropical China showed an increasing trend, with five extreme droughts recorded, of which 2011 was the most severe one; 2) the simulated average carbon storage of the EBF and ENF during 1985-2019 were 130.58 t·hm -2 and 78.49 t·hm -2 , respectively.

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