Ocean surface tipping point could accelerate climate change
The alkalinity-climate feedback. This schematic illustration shows how changes in upper-ocean density stratification and the ocean carbon cycle respond to increased atmospheric CO2 and feedback on one another to produce an amplified response on multi-century timescales. A vertical red arrow indicates an increase in that variable, while a vertical dark blue arrow indicates a decrease. Credit: Geophysical Research Letters (2023). DOI: 10.1029/2022GL101954…