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Progress in Earth and Planetary Science
Fig. 5 | Progress in Earth and Planetary Science

Fig. 5

From: δ18O and SST signal decomposition and dynamic of the Pliocene-Pleistocene climate system: new insights on orbital nonlinear behavior vs. long-term trend

Fig. 5

Time-series panel of the five SST components isolated from the ODP Site 846 record by singular spectrum analysis with the SST-filtered record (left) obtained by combining these data components (99.6% total variance). The x-axis scale (°C) is variable in relation to the component’s variance fraction. Original SST data from Herbert et al. (2010b) resampled at 1 kyr. Time scale in kyr

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