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Abstract Winter sea surface temperature (SST) in the South China Sea is a precursor of North China hydroclimate, but the relationship’s long-term stability remains uncertain. Using monthly resolved Xisha coral Sr/Ca-SST and three hydroclimate reconstructions analyzed at native temporal resolution, we find that the Medieval Climate Anomaly (MCA, 1149–1205 CE) is the only sampled interval with a cross-proxy-consistent positive relationship.
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