Uniformly elevated future heat stress in China driven by spatially heterogeneous water vapor changes.

However, southern China witnesses a decreasing trend in evaporation (Fig. 3A ) alongside a concurrent trend of moisture divergence (Fig. 3B ).

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S 25A ), and there was a shift in the trend of T w variations from a decreasing trend to an increasing trend after the late-1970s (Supplementary Fig.

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