Seasonally resolved surface water DC variability in the Lombok Strait: A coralline perspective

[1] We have explored surface water mixing in the Lombok Strait through a bimonthly resolved surface water DC time series reconstructed from a coral in the Lombok Strait that spans 1937 through 1990. The prebomb surface water DC average is 60.5%, and individual samples range from 72% to 134%. The annual average postbomb maximum occurs in 1973 at 122%. The timing of the postbomb maximum is consistent with a primary subtropical source for the surface waters in the Indonesian seas. During the postbomb period, the coral records regular seasonal cycles of 5% to 20%. Seasonal high DC occur during March–May (warm, low salinity), and low DC occur in September (cool, higher salinity). The DC seasonality is coherent and in phase with the seasonal DC cycle observed in Makassar Strait. We estimate the influence of highDC Makassar Strait (North Pacific) water flowing through the Lombok Strait using a two end-member mixing model and the seasonal extremes observed at the two sites. The percentage of Makassar Strait water varies between 16% and 70%, and between 1955 and 1990, it averages at 40%. The rich DC variability has a biennial component reflecting remote equatorial Indian Ocean forcing and a component in the ENSO band, which is interpreted to reflect Pacific forcing on the DC signature in Lombok Strait. Citation: Guilderson, T. P., S. Fallon, M. D. Moore, D. P. Schrag, and C. D. Charles (2009), Seasonally resolved surface water DC variability in the Lombok Strait: A coralline perspective, J. Geophys. Res., 114, C07029, doi:10.1029/2008JC004876.