This Bern model incorporates
non-linear ocean chemistry feedbacks and CO2 fertilization of the terrestrial biosphere, but it omits climate - carbon feedbacks, e.g., assuming static global climate and ocean circulation.
This Bern model incorporates
non-linear ocean chemistry feedbacks and CO2 fertilization of the terrestrial biosphere, but it omits climate - carbon feedbacks, e.g., assuming static global climate and ocean circulation.
CO2 is taken up in higher latitudes, mostly in the Southern
Ocean, but while the uptake rate is a non-linear function of the chemistry, ocean biology and circulation, it isn't going to «saturate» any time soon (though it may slow over the next few deca
Ocean, but while the uptake rate is a
non-linear function of the
chemistry,
ocean biology and circulation, it isn't going to «saturate» any time soon (though it may slow over the next few deca
ocean biology and circulation, it isn't going to «saturate» any time soon (though it may slow over the next few decades).