A best
estimate of climate sensitivity close to 3 °C for doubled CO2 has been inferred from paleoclimate data [51]--[52].
A best
estimate of climate sensitivity close to 3 °C for doubled CO2 has been inferred from paleoclimate data [51]--[52].
Not exact matches
«the long fat tail that is characteristic
of all recent
estimates of climate sensitivity simply disappears, with an upper 95 % probability limit... easily shown to lie
close to 4 °C, and certainly well below 6 °C.»
The
climate sensitivity is
closest associated with, for which the mean
estimate was 1.11, with a 5 -95-percentile interval
of 0.74 - 1.62.
Is there any indication
of acknowledgement
climate sensitivity may be
closer to the Forster / Gregory06
estimate (not the IPCC replot) than the IPCC AR4 concluded?
Anyone reading our paper may or may not agree with our choice
of parameters and hence with our revised
estimates of climate sensitivity, which are very much lower and very much
closer to observed reality than those
of the more complex models.
Would the lower rate
of cooling give us something
close to an empirical
estimate of climate sensitivity to increased CO2?
However, because
climate scientists at the time believed a doubling
of atmospheric CO2 would cause a larger global heat imbalance than today's
estimates, the actual
climate sensitivities were approximatly 18 % lower (for example, the «Best» model
sensitivity was actually
closer to 2.1 °C for doubled CO2).
However, as in the FAR, because
climate scientists at the time believed a doubling
of atmospheric CO2 would cause a larger global heat imbalance than current
estimates, the actual «best
estimate» model
sensitivity was
closer to 2.1 °C for doubled CO2.
Although below the model ECS
of 2.3 C, that is very
close to the GISS - E2 - R effective
climate sensitivity of ~ 2 C, which is what this method would
estimate if the forcing were purely from CO2.
The fact that others have created pdfs from
sensitivity estimates and that economists uses these pdfs is not a justification; rather,
climate researchers and statisticians need to take a
close look at this to see whether this line
of reasoning is flawed.
If one attributes half
of the observed warming (instead
of only 7 %) to natural forcing, this would put the 2xCO2
climate sensitivity at 0.8 °C, or very
close to the Lindzen and Spencer
estimates.
The reason to keep doing the science, as with the new article suggesting recent increasing transfer
of surface heat to the deep Atlantic, is to get a
closer estimate of climate sensitivity, which will then help narrow the choice
of policy options.
There have been a number
of new papers that use recent atmospheric, ocean, and surface temperature observations to argue that
climate sensitivity may be lower than previously
estimated (e.g.
closer to 2 C than 4 C).
Contrary to Schlesinger's result, the majority
of state -
of - the - art four - dimensional «general circulation models» (GCMs)- the kind used in the Trenberth and Fasullo study -
estimate the
climate sensitivity is
closer to 3 degrees C.
In discussion
of the
climate sensitivity to doubled atmospheric CO2 concentration, the combined subjective and objective criteria are explained: the range
of model results was 1.9 °C to 5.2 °C; most were
close to 4.0 °C; but the newer model results were lower; and hence the best
estimate was 2.5 °C with a range
of 1.5 °C to 4.5 °C.
The lower value — which conforms rather more closely with mainstream thinking than the higher value yields an effective
climate sensitivity of ca 1.5 deg K for a doubling
of CO2, which gets fairly
close to ZDM
estimates using historical forcing, temperature and ocean heat data.»
At first look I would think this is more like an
estimate of transient
climate sensitivity (and it happens to be
close to the IPCC number for TCS).
But again he was lucky: picking ~ 2ºC rather than the more likely ~ 3ºC
climate sensitivity compensates roughly for this, so his 20th - Century warming
of 0.8 ºC is almost spot on (the actual
estimate being
closer to 0.7 ºC, see Fig.