Ocean Acidification
The long-term shift in seawater carbonate chemistry caused primarily by ocean uptake of anthropogenic carbon dioxide.
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Clear searchThe long-term shift in seawater carbonate chemistry caused primarily by ocean uptake of anthropogenic carbon dioxide.
The wind-, buoyancy- and tide-driven movement of seawater that redistributes heat, carbon, nutrients and momentum.
The framework that explains the motion of Earth's lithospheric plates and the concentration of geological activity at their boundaries.