http://journals.ametsoc.org/doi/abs/10.1175/JCLI-D-12-00751.1

If anthropogenic CO2 emissions cease, will atmospheric CO2 concentration
continue to increase?

Andrew H. MacDougall,* Michael Eby, and Andrew J. Weaver
Journal of Climate
DOI: 10.1175/JCLI-D-12-00751.1

Abstract
If anthropogenic CO2 emissions were to suddenly cease, the evolution of the
atmospheric CO2 concentration would depend on the magnitude and sign of
natural carbon sources and sinks. Experiments using Earth system models
indicate that overall carbon sinks dominate, such that upon cessation of
anthropogenic emissions, atmospheric CO2 levels decrease over time.
However, these models have typically neglected the permafrost carbon pool,
which has the potential to introduce an additional terrestrial source of
carbon to the atmosphere. Here we use the University of Victoria Earth
System Climate Model (UVic ESCM), which has recently been expanded to
include permafrost carbon stocks and exchanges with the atmosphere. In a
scenario of zeroed CO2 and sulphate aerosol emissions, we assess whether
the warming induced by specified constant concentrations of
non-CO2 greenhouse gases could slow the CO2 decline following zero
emissions, or even reverse this trend and cause CO2 to increase over time.
We find that a radiative forcing from non-CO2 gases of approximately 0.6 W
m-2 results in a near balance of CO2 emissions from the terrestrial
biosphere and uptake of CO2 by the oceans, resulting in near-constant
atmospheric CO2 concentrations for at least a century after emissions are
eliminated. At higher values of non-CO2 radiative forcing,
CO2 concentrations increase over time, regardless of when emissions cease
during the 21st century. Given that the present-day radiative forcing from
non-CO2 greenhouse gases is about 0.95 W m-2, our results suggest that if
we were to eliminate all CO2and aerosols emissions without also decreasing
non-CO2greenhouse gas emissions, CO2 levels would increase over time,
resulting in a small increase in climate warming associated with this
positive permafrost carbon feedback.

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