There's typically
an initial ocean uptake as tropical East Pacific upwelling (CO2 degassing) is reduced, followed by a stronger release of carbon from land.
Not exact matches
If I instantly quadruple CO2 in an experiment, I'd expect
ocean heat
uptake (OHU) to occur pretty uniformly in latitude for the
initial few years, but then become pretty localized to the subpolar
oceans after, say, year 100.
If I instantly quadruple CO2 in an experiment, I'd expect
ocean heat
uptake (OHU) to occur pretty uniformly in latitude for the
initial few years, but then become pretty localized to the subpolar
oceans after, say, year 100.
The same holds for human CO2 releases: an
initial increase in atmospheric CO2 levels will lead to increased
uptake by the
oceans and biosphere, but a part of the increase will remain in the atmosphere, as long as CO2 is constantly added.