For example, current models are highly inconsistent in the way they treat the response of Net Primary Production (NPP) to climate variability and climate change even though this response is fundamental to predictions of the total
terrestrial carbon balance in a changing climate.
Not exact matches
By 2100, the ocean uptake rate of 5 Gt C yr - 1 is
balanced by the
terrestrial carbon source, and atmospheric CO2 concentrations are 250 p.p.m.v. higher in our fully coupled simulation than in uncoupled
carbon models2, resulting in a global - mean warming of 5.5 K, as compared to 4 K without the
carbon - cycle feedback.
The
carbon balance shows that
terrestrial biomass and soil nets an extra 3 Gt C per year, so only 60 - 70 % of emissions remain, ~ 6 Gt C, as ghg's and ocean acidifying H2CO3.
The existence of this oceanic
carbon pump also raises questions about the need for a large
terrestrial carbon sink in the Northern Hemisphere, as postulated by Tans et al. 3, to
balance the present global
carbon budget.
For the thousandth time, there is a
CARBON CYCLE (open your ears this time), which means that carbon is cycled through the oceans, terrestrial biosphere and atmosphere and stays in rough balance with what is absorbed and em
CARBON CYCLE (open your ears this time), which means that
carbon is cycled through the oceans, terrestrial biosphere and atmosphere and stays in rough balance with what is absorbed and em
carbon is cycled through the oceans,
terrestrial biosphere and atmosphere and stays in rough
balance with what is absorbed and emitted.
Changes in vegetation
carbon residence times can cause major shifts in the distribution of
carbon between pools, overall fluxes, and the time constants of
terrestrial carbon transitions, with consequences for the land
carbon balance and the associated state of ecosystems.
The reason for a reduced CO2 rate of rise was probably not due to a reduction in emission rates, but it may have reflected
carbon cycle feedbacks that slightly altered the
balance between atmospheric CO2 and
terrestrial and oceanic sinks.