Although the linear precipitation trend in southeastern China is barely significant at the 80% level, an increasing (decreasing) precipitation in summer rainfall is evident over southeastern (northeastern) China from 1985–1994 to 2001–2010 ( Fig. 2B ).
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Effect of anthropogenic sulphate aerosol in China on the drought in the western-to-central US.
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Furthermore, a negative trend of precipitation in the western-to-central US for 1985–2010 is also found ( Supplementary Fig.
In addition, the total precipitation variability from the CMAP observations shows an increasing trend of summer precipitation in southeastern China for 1985–2010 ( Fig. 2A ).