Various mechanisms have been proposed for this hiatus in global warming3, 4,5,6, but their relative importance has not been quantified, hampering
observational estimates of climate sensitivity.
B) Im interested because the temperature record is important to
observational estimates of climate sensitivity.
Observational estimates of climate sensitivity from changes in the rate of ocean heat uptake and comparison to CMIP5 models.
- that new estimates of aerosol cooling are low - that new estimates of Ocean heat uptake are low - that therefore
observational estimates of climate sensitivity may prove low - that observational estimates are now good enough that they should be preferred over models - that warming below 2C is net beneficial
Not exact matches
Since we can not do controlled experiments,
climate science is an
OBSERVATIONAL science we can't put the
climate in a beaker, we can only look at past temperatures and past forcings to CONSTRAIN our
estimate of sensitivity.
As these figures show,
estimates from both models and
observational data consistently find that the most likely
climate sensitivity value is approximately 3 °C for a doubling
of CO2.
«Lewis & Crok perform their own evaluation
of climate sensitivity, placing more weight on studies using «
observational data» than
estimates of climate sensitivity based on
climate model analysis.»
As a result, the study would provide little evidence that historical period
observational estimates of ECS have been biased low in relation to effective
climate sensitivity.
In context
of the way
climate sensitivity is defined by the IPCC, uncertainty in
climate sensitivity is decreasing as errors in previous
observational estimates are identified and eliminated and model
estimates seem to be converging more.
There are also a substantial number
of observational climate sensitivity estimates below 1 C. e.g. Lindzen & Choi (2009) at 0.5 C. See my comment on apparent bimodal distribution
of climate sensitivity estimates.
There are also a substantial number
of observational climate sensitivity estimates below 1 C, e.g. Lindzen & Choi (2009) at 0.5 C..
In the Working Group 1: The Physical Science Basis Report
of AR4 («AR4: WG1»), various studies deriving
estimates of equilibrium
climate sensitivity from
observational data are cited, and a comparison
of the results
of many
of these studies is shown in Figure 9.20, reproduced below.
The
observational constraint in Volodin (2008) suggests that
climate sensitivity more likely lies in the upper range
of model
estimates (ECS most likely around 3.5 K), in agreement with more recent studies by Siler et.
Fred, You write: «Ron — Every
climate sensitivity estimate that has ever been done has utilized models
of one sort or another, and all have also used
observational data.»
To better assess confidence in the different model
estimates of climate sensitivity, two kinds
of observational tests are available: tests related to the global
climate response associated with specified external forcings (discussed in Chapters 6, 9 and 10; Box 10.2) and tests focused on the simulation
of key feedback processes.
The 0C - 10C range for 2xCO2
climate sensitivity encompasses ALL the published
estimates I have seen, from the Spencer and Lindzen lower end
of 0.6 C (from CERES and ERBE satellite observations) and the Forster and Gregory range
of 0.9 C to 3.7 C (based on «purely
observational evidence» — see earlier thread) to IPCC's range
of 2.0 C to 4.5 C (from model simulations based largely on theoretical deliberations rather than physical observations).