But
ocean surface layers take nowhere near centuries to turn over.
Not exact matches
As temperatures rise today, most of the heat is being
taken up by the
surface layers of the
oceans.
As a result of this, more of the CO2 bound in organic matter remains in the
surface layer, which reduces the
ocean's potential to
take up atmospheric CO2.»
Stuck to their calcium carbonate platelets, organic matter sinks to the
ocean floor — allowing
surface layers to
take up a new carbon dioxide from the atmosphere and process it.
Balance time for those
surface layers is short, but for the deep
ocean, CO2 doesn't diffuse but is gradually carried there by slow moving
ocean currents, these may
take on the order of a thousand years to complete.
I'd like to ask a general question: since the
oceans are
taking up about 1/3 of the anthropogenic carbon emissions, what is the opinion now of the scientific community about when the
ocean surface layers will get saturated and this carbon sink (on relatively short timescales) will start to diminish?
Whether the
ocean surface warms more than that is totally dependent on how long it
takes excess
surface layer energy to be diluted into the entire basin.
It
takes about 1.5 years to bring the
oceans surface layer in equilibrium with the atmosphere.
When the
ocean surface is cooler, warmth is
taken from the
surface into deeper
ocean layers that «do not emit heat out of the planet».
Either this is a truism (the sun must be heating the
ocean surface first) or it is meant to
take into account the complex circulations that occur in the
ocean, like the Gulf Stream's involvement in a vertical rise of waters from deep
ocean layers in one region and sinking of the cooled
surface waters as the stream reaches its northern limit.
Of course, if the air were to be warmer than the
ocean surface then evaporation would
take the extra energy required from the air rather than the water and that 1 mm deep
layer (0.3 C cooler than the
ocean bulk) would rise to the
surface and dissipate but that doesn't happen often or for long.