INTERACTION BETWEEN THE ENSO AND THE ASIAN MONSOON IN A CORAL RECORD OF TROPICAL CLIMATE

The oxygen isotopic composition of a banded coral from the western equ atorial Indian Ocean provides a 150-year-long history of the relation between the El Nino-Southern Oscillation (ENSO) phenomenon and the Asi an monsoon. Interannual cycles in the coral time series were found to correlate with Pacific coral and instrumental climate records, suggest ing a consistent linkage across ocean basins, despite the changing fre quency and amplitude of the ENSO. However, decadal variability that is characteristic of the monsoon system also dominates the coral record, which implies important interactions between tropical and midlatitude climate variability. One prominent manifestation of this interaction is the strong amplitude modulation of the quasi-biennial cycle.