Responses of the summer Asian-Pacific zonal thermal contrast and the associated evolution of atmospheric circulation to transient orbital changes during the Holocene.

Its index presented an increasing trend, which implies the enhancement of a zonal thermal contrast between Asia and the North Pacific.

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The incoming solar radiation exhibits a decreasing trend in the warm season (May-August), with a maximum variation exceeding 32.5 W·m −2 , an increasing trend in the cold season (October-March), with a maximum variation exceeding 27.5 W·m −2 , and an increase (decrease) before 5 ka and a subsequent decrease (increase) in September (April).

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