Pacific freshening drives Pliocene cooling and Asian monsoon intensification.

However, from ~4.3 to 2.7 Ma, the χ ARM and χ ARM /SIRM records show increasing trends while the χ ARM /χ LF record shows a decreasing trend.

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In this case, χ ARM /SIRM and χ ARM will have an increasing trend, controlled dominantly by the effects of increasing precipitation ( Fig. 2d, 2f and Table 1 ), while χ ARM /χ LF will have a decreasing trend, attributed to the dominant effects of decreasing temperature ( Fig. 2a and Table 1 ).

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