Fig. 10From: δ18O and SST signal decomposition and dynamic of the Pliocene-Pleistocene climate system: new insights on orbital nonlinear behavior vs. long-term trendExponential relationships of the orbital variance of a δ18O components and b SST components vs. the average of component-1 exponential fit trends by time segments binned at 532 kyr. The right y-axis shows the variance of comp-2-11 (orbitals) with a different scale to not compress the left y-axis valuesBack to article page