However, over the entire time interval compared, maximum variations of mean summer SST are 1jC, which would account for approximately 0.20x in coral y18O (Juillet- Leclerc and Schmidt, 2001). Over the same period, mean summer coral y18O varies by as much as 0.7x (piM) and 0.4x (COI-5) (Fig. 4); i.e., the maximum SST contribution to the coral isotopic signal is 29% (piM) and 50% (COI-5)

Core GIM correlates more strongly with precipitation and OLR than COI-5 (Table 1). Note that years of high rainfall coincide with years of large negative coral y18O anomalies in the wet season (and high amplitudes of the annual cycle,

midpoint depth of the subsample drilled for UTh age

[230Th/238U] activity measured in the subsample

Analytical uncertainty of 230Th238U activity

Analytical uncertainty of 230Th232Th ratio

Calculated initial d234U in the subsample

Depth at the top of the subsample for 210Pb analysis

Depth at the bottom of the subsample for 210Pb analysis

Lead210 excess measured in the subsample

Depth at the top of the subsample for 137Cs analysis

Depth at the bottom of the subsample for 137Cs analysis

Cesium137 gactivity measured in the subsample

Analytical uncertainty of 137Cs gactivity

Need to aquire data for core GIM from authors, NCDC only has core COI5

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