A summary of
recent climate sensitivity studies can be found here.
Not exact matches
«This is one of several
recent studies that provide sobering evidence that earth's
climate sensitivity may lie in the upper end of the current uncertainty range,» Mann said in an email.
That
study addressed a puzzle, namely that
recent studies using the observed changes in Earth's surface temperature suggested
climate sensitivity is likely towards the lower end of the estimated range.
Therefore
studies based on observed warming have underestimated
climate sensitivity as they did not account for the greater response to aerosol forcing, and multiple lines of evidence are now consistent in showing that
climate sensitivity is in fact very unlikely to be at the low end of the range in
recent estimates.
One
recent study examining the Palaeocene — Eocene Thermal Maximum (about 55 million years ago), during which the planet warmed 5 - 9 °C, found that «At accepted values for the
climate sensitivity to a doubling of the atmospheric CO2 concentration, this rise in CO2 can explain only between 1 and 3.5 °C of the warming inferred from proxy records» (Zeebe 2009).
Do you think that in the same way that the Solanki et al paper on solar sunspot reconstructions had a specific statement that their results did not contradict ideas of strong greenhouse warming in
recent decades, this (the fact that
climate sensitivity projections are not best estimates of possible future actual temperature increases) should be clearly noted in media releases put out by scientists when reporting
climate sensitivity studies?
Interestingly, our results are actually pretty consistent with a lot of the
recent literature on
sensitivity: All
studies comparing simple models with
recent climate change (from Andronova and Schlesinger, 2001, onwards) find high
sensitivities (more than 8K, say) are consistent (at the few - percent level) with the observed record unless they are ruled out a priori.
That
study addressed a puzzle, namely that
recent studies using the observed changes in Earth's surface temperature suggested
climate sensitivity is likely towards the lower end of the estimated range.
Therefore
studies based on observed warming have underestimated
climate sensitivity as they did not account for the greater response to aerosol forcing, and multiple lines of evidence are now consistent in showing that
climate sensitivity is in fact very unlikely to be at the low end of the range in
recent estimates.
The first paper adds to the literature pointing to humans as the dominant cause of warming since 1950, but also finds that the
sensitivity of the
climate system to the greenhouse - gas buildup could be lower than some other
recent studies found.
In Addendum:
Climate Change Impacts in the United States (pp. 26 - 28), Michaels and his colleague Chip Knappenberger discuss those studies in greater detail and also illustrate with two graphs how the IPCC AR4 warming projections should be adjusted in light of more recent climate sensitivity re
Climate Change Impacts in the United States (pp. 26 - 28), Michaels and his colleague Chip Knappenberger discuss those
studies in greater detail and also illustrate with two graphs how the IPCC AR4 warming projections should be adjusted in light of more
recent climate sensitivity re
climate sensitivity research.
The manuscript uses a simple energy budget equation (as employed e.g. by Gregory et al 2004, 2008, Otto et al 2013) to test the consistency between three
recent «assessments» of radiative forcing and
climate sensitivity (not really equilibrium
climate sensitivity in the case of observational
studies).
His
study and other
recent research, he said, suggests that «we may need to go back and start recalculating the
climate sensitivity estimates for the earth.»
(The
recent lowering of
climate sensitivity from 3 degrees to something on the order of 1.6 degrees in multiple
studies is a welcome development.)
As we discussed regarding the Norwegian paper,
studies estimating
climate sensitivity based on
recent data may be biased low due to a failure to account for increased heat transfer to the 700 — 2000 meter ocean layer (Figure 3).
That is why I consider the conclusion of MEA15, that «
Climate sensitivities estimated from
recent observations will therefore be biased low...» to be unjustifiable, whether or not the
study contains serious errors (as it does).
Our results agree with
recent studies that annual mean data - constraints from present day
climate prove to not rule out
climate sensitivities above the widely assumed
sensitivity range of 1.5 — 4.5 °C (Houghton et al. 2001).
I'm afraid you are barking up the wrong tree when you simply tell me all the
recent studies showing a much lower 2xCO2 equilibrium
climate sensitivity are In your opinion «all wrong» (and actually expect me to believe you).
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.
2) Other
studies are confirming a low
climate sensitivity to CO2 doubling around 1 C, as the
recent paper by Spencer.
Combined LGM, Eemian and Pliocene
studies would address an issue raised at a
recent workshop [99]: the need to evaluate how
climate sensitivity varies as a function of the initial
climate state.
Kevin Dayaratna's testimony favored low probability distributions for
climate sensitivity, all based on empirical
studies of
recent warming.
The TSD purports to rely on IPCC work as a basis for a supposed «
sensitivity» of
climate to increasing atmospheric C02, but fails to mention that the most
recent IPCC report completely undermines any basis for determining
climate sensitivity with the following statement: «No best estimate for equilibrium
climate sensitivity can now be given because of a lack of agreement on values across assessed lines of evidence and
studies.»
A
recent study used NASA satellite observations to test the skill of
climate models in simulating this cloud - type transition, and found that high
sensitivity models simulate it more accurately, while low
sensitivity models tend to overemphasize its
climate cooling effect.
A
recent study by C10 analysed a number of different
climate variables in a set of SMEs of HadCM3 (Gordon et al. 2000, atmosphere — ocean coupled version of HadSM3) from the point of view of global - scale model errors and
climate change forcings and feedbacks, and compared them with variables derived from the CMIP3 MME. Knutti et al. (2006) examined another SME based on the HadSM3 model, and found a strong relationship between the magnitude of the seasonal cycle and
climate sensitivity, which was not reproduced in the CMIP3 ensemble.
In which case please point to a significant cluster of
recent studies (preferably, but not necessarily, based upon observations) which support higher estimates of
climate sensitivity.
As well as this simple estimate from heat balance implying a best estimate for ECS of approximately 1.6 °C, and the reworking of the Gregory 02 results suggesting a slightly lower figure, two good quality
recent observationally - constrained
studies using relatively simple hemispheric - resolving models also point to
climate sensitivity being about 1.6 °C:
As valuation depends strongly on the transient
climate response, uncertainty in
sensitivity is based on the range in a
recent study of the AR5 models (1.3 — 3.15 °C; (Shindell 2014)-RRB- relative to the mean of those models (1.8 °C, hence − 28 % / +75 %; those models also exhibited a mean ECS of 3.2 °C).
Empirical data from
recent studies based on actual physical observations have raised serious doubt concerning these feedback assumptions and the resulting 2xCO2
climate sensitivity.