Fig. 2: Power spectra of coral Sr/Ca, δ18O, and instrumental SST. | Communications Earth & Environment

Fig. 2: Power spectra of coral Sr/Ca, δ18O, and instrumental SST.

From: Strontium to calcium ratio and oxygen isotopic coral records can exaggerate past decadal tropical climate variability

Fig. 2: Power spectra of coral Sr/Ca, δ18O, and instrumental SST.

a A comparison of the uncorrected (Sproxy) and corrected (Sclim) spectra estimated from coral Sr/Ca and δ18O with the power spectral density (PSD) of instrumental SST (ERSSTv5 & OISSTv2) evaluated for the locations and time periods for which there were Sr/Ca and δ18O data. Spectra represent averages across all pairs of coral records analyzed in this study. For a and b, units have been converted to Kelvin by multiplying Sr/Ca and δ18O based spectra by 1/0.062 and 1/0.222 respectively. b No. of pairs and the number of unique records contributing to the mean power spectra at each frequency for coral derived data. c Power spectral density of the uncorrected coral proxy records, shared (climate) and noise components estimated using the stacked records method. For proxy-based power spectra, shaded regions indicate 68 and 95% confidence intervals estimated by record-wise bootstrapping. Bootstrapped interval estimation was not possible for timescales with contributions from less than about 20 coral pairs (the precise number was dependent on the variation of the given statistic).

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