Why are Surface Ocean pH and CaCO<sub>3</sub> Saturation State Often out of Phase in Spatial Patterns and Seasonal Cycles?

Although both pH and calcium carbonate mineral saturation states (Ω) are good metrics for ocean acidification, in the global surface ocean their spatial patterns and seasonal cycles are often out of phase, which appears counter intuitive. To explain this, we separate pH and Ω changes into thermal and nonthermal components. Thermal components are mainly related […]

Why are Surface Ocean pH and CaCO<sub>3</sub> Saturation State Often out of Phase in Spatial Patterns and Seasonal Cycles? Read More »