Indian Ocean Dipole. A modern coral covers the period from 1968 to 2007. A sub-fossil coral
derives from the medieval climate anomaly (MCA) and spans 1100–1140 ad. The modern
coral records SST variability in the eastern pole of the Indian Ocean Dipole. A strong
correlation is also found between coral Sr/Ca and the IOD index. The correlation with ENSO
is asymmetric: the coral shows a moderate correlation with El Niño and a weak correlation …