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Fig. 3 | Progress in Earth and Planetary Science

Fig. 3

From: Millennial-scale variability of East Asian summer monsoon inferred from sea surface salinity in the northern East China Sea (ECS) and its impact on the Japan Sea during Marine Isotope Stage (MIS) 3

Fig. 3

Comparison among the results with three different calibrations for KR07-12 PC-01: “No salinity correction” (gray), “salinity correction” (red), and “endmember correction” (blue). a δ18O of planktic foraminifer (δ18Op). b SST. c δ18Ow-local. d SST vs. δ18Ow-local derived from “no salinity correction” calibration method. e SST vs. δ18Ow-local derived from “salinity correction” calibration method

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