Fig. 4: Precession-dominated hydrological changes in the low to mid-latitudes of Eastern Asia.
From: Late Pleistocene island weathering and precipitation in the Western Pacific Warm Pool

a, b, and c are the same as in Fig. 2. d Stacked surface seawater oxygen isotope (δ18Osw) and stacked ocean heat content (OHC) anomaly, both from the Indo-Pacific Warm Pool (IPWP)29. e Stalagmite δ18O records from Sanbao Cave as an indicator of the East Asian Summer Monsoon5, and insolation gradient from 30 °N to 30 °S in June66. Precessional cycles are indicated, with light blue bars representing precession minima.