However, the models also suggest that, as we go forward in time, the relative importance of increasing radiative effects, compared with atmosphere and
ocean dynamic effects, is likely to increase.
Not exact matches
Here we quantify the
effects of key parametric uncertainties and observational constraints on thermosteric SLR projections using an Earth system model with a
dynamic three - dimensional
ocean, which provides a mechanistic representation of deep
ocean processes and heat uptake.
SAL
effects produce additional variations in
ocean mass ranging from a few mm to more than 1 cm and can be of the same order of magnitude as the variations in
dynamic bottom pressure in several
ocean regions.
The above also is true for the opposite
effect: if there were no other fast releases (like lots of volcanoes spewing lots of CO2 in short time), the
ocean temperature will give more or less CO2, until a new
dynamic equilibrium between
ocean releases (mainly near the tropics) and sinks (mainly near the poles) and the biosphere releases and sinks is reached.