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In reference to our recent paper (1), Yu et al. (2) maintain that (i) increased anthropogenic aerosols caused a weakening of the East Asian summer monsoon (EASM) over the past few decades, together with a concomitant “southern-flood-northern-drought” (SFND) pattern in China, and (ii) our finding of a warming-induced northward shift of the EASM from the Last Glacial Maximum (LGM) to the Holocene is not applicable to the present case. Atmospheric aerosols, formed from both natural and anthropogenic sources, may affect the climate in multiple and complex ways through their interactions with radiation and clouds (3). However, the impact of aerosols on regional climate is fraught with uncertainties (3). Yu …

Reply to Yu et al.: Global temperature change as the ultimate driver of the shift in the summer monsoon rain belt in East Asia