When extra forcing of -0.25 or -0.5 W / m ^ 2 is added his prior
mean total aerosol forcing is very substantially more negative than -0.7 W / m ^ 2 (the posterior mean without the extra indirect forcing).
This is not the subject but it seems that, in AR5 (sorry it is the leaked version),
the mean total aerosol forcing is less (30 %) than this same forcing in AR4.
When extra forcing of -0.25 or -0.5 W / m ^ 2 is added his prior
mean total aerosol forcing is very substantially more negative than -0.7 W / m ^ 2 (the posterior mean without the extra indirect forcing).
Not exact matches
Of these, the smallest best estimate I can find is -0.85 W / m ^ 2, which
means the reported -0.7 is unlikely to be representative of
total aerosol forcing, whatever else it relates to.
The one slightly fortuitous aspect to this is that the forcing from CO2 alone is around 1.5 W / m2, while if you add up all of the forcings, including warming factors (like CO2 and CH4) and cooling factors (like
aerosols), you end up with a
total around 1.6 W / m2 — i.e. all of the extra stuff we've put in over the years pretty much cancels out in the global
mean.
I was interested in the quantitative order of the
mean overestimation of the
total effective
aerosol forcing (ERFaero) of the CMIP5 models.
PS to my 4:48 AM post: The non-linearity of the TCR estimate to
aerosol forcing also
means that a 0.49 W / m2
total adjustment would bring the TCR estimate down to about 1.4 °C, not 1.26 °C (which was based on a simple scaling of Shindell's sensitivity analysis).
With the posterior
mean less negative than the 95 % point of the prior, the observational data must be pointing to an even less negative
total aerosol AF estimate than -0.8 W / m ^ 2, with the wing of the prior pulling the posterior to a more negative
mean.
Of these, the smallest best estimate I can find is -0.85 W / m ^ 2, which
means the reported -0.7 is unlikely to be representative of
total aerosol forcing, whatever else it relates to.