But it does point to a number
of climate sensitivity studies — empirical and otherwise — within the last few years.
Curry provides a highly biased and skewed overview
of climate sensitivity studies, which makes sense for publication in the Wall Street Journal.
Not exact matches
Some
studies of past
climate, however, point to
climate sensitivities of 6 °C or more.
Earlier
studies on the
sensitivity of tropical cyclones to past
climates have only analyzed the effect
of changes in the solar radiation from orbital forcing on the formation
of tropical cyclones, without considering the feedbacks associated to the consequent greening
of the Sahara.
«We may have to wait 20 or 30 years before the data set in the 21st century is good enough to pin down
sensitivity,» says
climate modeler Gavin Schmidt
of the NASA Goddard Institute for Space
Studies (GISS).
At the same time, new
studies of climate sensitivity — the amount
of warming expected for a doubling
of carbon dioxide levels from 0.03 to 0.06 percent in the atmosphere — have suggested that most models are too sensitive.
To estimate how much the
sensitivity varies, Gary Russell
of the NASA Goddard Institute for Space
Studies in New York and colleagues ran a
climate model repeatedly.
«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.
Based on past observations, Held, who was not involved with the
study, said the
climate sensitivity of 5 °C or more shown by the new research may be implausible.
By
studying the relationship between CO2 levels and
climate change during a warmer period in Earth's history, the scientists have been able to estimate how the
climate will respond to increasing levels
of carbon dioxide, a parameter known as «
climate sensitivity».
The
sensitivity of leaf unfolding phenology to
climate warming has significantly declined since 1980s, according to a
study recently published in the journal Nature by an international collaboration
of scientists.
«Thus it appears that the Pinatubo cooling favours high
climate sensitivity,» say Hansen and his colleagues in a
study for a forthcoming issue
of the journal National Geographic Research and Exploration.
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.
The NGN article itself gives a good explanation
of climate sensitivity and the various
studies and estimates
of it, and does quote Michael Schlesinger
of the University
of Illinois saying that Hegerl's result «means
climate sensitivity is larger than we thought for 30 years, so the problem is worse than we thought.
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.
National Geographic News reports that this week's issue
of Nature will publish a
study from a team led by Gabriele Hegerl
of Duke University which finds
climate sensitivity of 1.5 º to 6.2 ºC, with a higher end somewhat higher than the standard range
of 1.5 — 4.5 ºC.
Sure, there might be a few papers that take
climate sensitivity as a given and somehow try to draw conclusions about the impact on the
climate from that... But, I hardly think that these are swamping the number
of papers trying to determine what the
climate sensitivity is,
studying if the water vapor feedback is working as expected, etc., etc..
Such
studies can reasonably account for the observed variations as a response to solar and volcanic forcing (and a few secondary things) with energy balance
climate models tuned to have a
climate sensitivity equivalent to 2.5 C per doubling
of CO2.
Therefore, I wouldn't attach much credence, if any, to a modelling
study that didn't explore the range
of possibilities arising from such uncertainty in parameter values, and particularly in the value
of something as crucial as the
climate sensitivity parameter, as in this example.
A summary
of recent
climate sensitivity studies can be found here.
Several
studies have put the lower bound
of climate sensitivity at about 1.5 °C, on the other hand, several others have found that a
sensitivity higher than 4.5 °C can't be ruled out.
It is important to regard the LGM
studies as just one set
of points in the cloud yielded by other
climate sensitivity estimates, but the LGM has been a frequent target because it was a period for which there is a lot
of data from varied sources,
climate was significantly different from today, and we have considerable information about the important drivers — like CO2, CH4, ice sheet extent, vegetation changes etc..
This is a 0.9 ºC reduction from the
sensitivity of 2.5 °C estimated in that predecessor
study, which used the same
climate model.
Given that clouds are known to be the primary source
of uncertainty in
climate sensitivity, how much confidence can you place in a
study based on a model that doesn't even attempt to simulate clouds?
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).
One
of his reasons to claim that «the risk
of catastrophic anthropogenic global warming appears to be so low that it is not currently worth doing anything to try to control it» is that he uses a very low value for the
climate sensitivity based on non-reviewed «
studies», while ignoring the peer - reviewed work.
The IPCC AR4 (9.6: Observational Constraints on
Climate Sensitivity) lists 13 studies (Table 9.3) that constrain climate sensitivity using various types of data, including two using LG
Climate Sensitivity) lists 13 studies (Table 9.3) that constrain climate sensitivity using various types of data, including two usin
Sensitivity) lists 13
studies (Table 9.3) that constrain
climate sensitivity using various types of data, including two using LG
climate sensitivity using various types of data, including two usin
sensitivity using various types
of data, including two using LGM data.
Absent understanding
of cloud feedback processes, the best you can really do is mesh it into the definition
of the emergent
climate sensitivity, but I think probing (at least some
of) the uncertainties in effects like this is one
of the whole points
of these ensemble - based
studies.
They conclude, based on
study of CMIP5 model output, that equilibrium
climate sensitivity (ECS) is not a fixed quantity — as temperatures increase, the response is nonlinear, with a smaller effective ECS in the first decades
of the experiments, increasing over time.
These models all suggest potentially serious limitations for this kind
of study: UVic does not simulate the atmospheric feedbacks that determine
climate sensitivity in more realistic models, but rather fixes the atmospheric part
of the
climate sensitivity as a prescribed model parameter (surface albedo, however, is internally computed).
My main criticism
of their
study is that they have calculated effective
climate sensitivity (their ICS) on a basis which is wrong for ICS in GCMs; their basis is also inconsistent with observationally - based estimates
of ICS.
The
study of past warm
climates may not narrow uncertainty in future
climate projections in coming centuries because fast
climate sensitivity may itself be state - dependent» http://www.pnas.org/content/110/35/14162.full
Inverse estimates
of aerosol forcing from detection and attribution
studies and
studies estimating equilibrium
climate sensitivity (see Section 9.6 and Table 9.3 for details on
studies).
d Explores IPCC TAR range
of climate sensitivity (i.e., 1.5 °C to 4.5 °C), while other
studies explore wider ranges
Climate model studies and empirical analyses of paleoclimate data can provide estimates of the amplification of climate sensitivity caused by slow feedbacks, excluding the singular mechanisms that caused the hyperthermal
Climate model
studies and empirical analyses
of paleoclimate data can provide estimates
of the amplification
of climate sensitivity caused by slow feedbacks, excluding the singular mechanisms that caused the hyperthermal
climate sensitivity caused by slow feedbacks, excluding the singular mechanisms that caused the hyperthermal events.
«We indicated 23 years ago — in our 1994 Nature article — that
climate models had the atmosphere's
sensitivity to CO2 much too high,» said Christy, the lead author in the
study, which has been accepted for publication in the 2017 fourth quarter edition
of the Asia - Pacific Journal
of Atmospheric Sciences and is available online.
Other AgMIP initiatives include global gridded modeling, data and information technology (IT) tool development, simulation
of crop pests and diseases, site - based crop -
climate sensitivity studies, and aggregation and scaling.
National Geographic News reports that this week's issue
of Nature will publish a
study from a team led by Gabriele Hegerl
of Duke University which finds
climate sensitivity of 1.5 º to 6.2 ºC, with a higher end somewhat higher than the standard range
of 1.5 — 4.5 ºC.
The aim
of this
study is to investigate the impact
of small - scale atmospheric fluctuations on the modeled
climate sensitivity to increased CO2 concentration.
One can temper that with
studies of paleoclimate
sensitivity, but the ensemble results still should be borne in mind, since doubling CO2 takes us into a
climate that has no real precendent in the part
of the
climate record which has been used for exploring model
sensitivity, and in many regards may not have any real precedent in the entire history
of the planet (in terms
of initial condition and rapidity
of GHG increase).
Actually Olson et al's abstract states «Our results are consistent with most previous
studies» and «The mode
of the
climate sensitivity estimate is 2.8 °C, with the corresponding 95 % credible interval ranging from 1.8 to 4.9 °C» (which supports the first quote).
The NGN article itself gives a good explanation
of climate sensitivity and the various
studies and estimates
of it, and does quote Michael Schlesinger
of the University
of Illinois saying that Hegerl's result «means
climate sensitivity is larger than we thought for 30 years, so the problem is worse than we thought.
eg «These
studies provide new insights on the
sensitivity and response
of meridional ocean circulation to melt water inputs to the North Atlantic high latitudes (e.g., Bamberg et al., 2010; Irvali et al., 2012; Morley et al., 2011) and their potential role in amplifying small radiative variations into large a
climate response through dynamic changes in ocean - atmosphere interactions (e.g., Morely et al., 2011; Irvali et al., 2012; Morley et al., 2014).
Finally, there is no good reason to widen the range, even though some
studies have pointed to the possibility
of higher
climate sensitivity — but as we have discussed here, they did not provide positive evidence for a higher
climate sensitivity, they merely showed that the data constraints used were weak.
But what the GSL now says is that geological evidence from palaeoclimatology (
studies of past
climate change) suggests that if longer - term factors are taken into account, such as the decay
of large ice sheets, the Earth's
sensitivity to a doubling
of CO2 could itself be double that predicted by most
climate models.
Based on many
studies covering a wide range
of regions and crops, negative impacts
of climate change on crop yields have been more common than positive impacts (high confidence)... Since AR4, several periods
of rapid food and cereal price increases following
climate extremes in key producing regions indicate a
sensitivity of current markets to
climate extremes among other factors (medium confidence).
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?
Hence, we feel that the most important result
of the
study of Stainforth et al. is that by far most
of the models had
climate sensitivities between 2ºC and 4ºC, giving additional support to the widely accepted range (Update: As mentioned in the follow up post, this clustering is mainly a function
of the
sensitivity of the original model and the random nature
of the perturbations).
«The closest match, with a much lower degree
of uncertainty than most other
studies, suggests
climate sensitivity is about 2.4 degrees.»
One
of his reasons to claim that «the risk
of catastrophic anthropogenic global warming appears to be so low that it is not currently worth doing anything to try to control it» is that he uses a very low value for the
climate sensitivity based on non-reviewed «
studies», while ignoring the peer - reviewed work.