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Climate change feedbacks on future oceanic acidification
2007
Tellus: Series B, Chemical and Physical Meteorology
A B S T R A C T Oceanic anthropogenic CO 2 uptake will decrease both the pH and the aragonite saturation state ( arag ) of seawater leading to an oceanic acidification. However, the factors controlling future changes in pH and arag are independent and will respond differently to oceanic climate change feedbacks such as ocean warming, circulation and biological changes. We examine the sensitivity of these two CO 2 -related parameters to climate change feedbacks within a coupled atmosphere-ocean
doi:10.1111/j.1600-0889.2006.00241.x
fatcat:pixghxhuhbe2jd3yipw6ojr74y