Could some aspect of our situation, e.g. the extreme rapidity of the forcing change, be sufficiently novel to make Earth's climate respond differently than it has in the past, and could this cause divergence from models based on
paleoclimate sensitivity estimates?
Not exact matches
A best
estimate of climate
sensitivity close to 3 °C for doubled CO2 has been inferred from
paleoclimate data [51]--[52].
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 events.
David's comments reminded me of something that Suki Manabe and I wrote more than 25 years ago in a paper that used CLIMAP data in a comparative evaluation of two versions of the 1980s - vintage GFDL model: «Until this disparity in the
estimates of LGM
paleoclimate is resolved, it is difficult to use data from the LGM to evaluate differences in low latitude
sensitivity between climate models.»
The
estimate for the CO2
sensitivity comes (mostly) from
paleoclimate studies, observed climate responses to volcanoes, and climate models.
This means that approaches that use the first order approximation to
estimate climate
sensitivity from the instrumental period (such as Lewis) will underestimate climate
sensitivity and approaches that use the first order to
estimate climate
sensitivity using
paleoclimate data (Hansen and others) will overestimate climate
sensitivity.
A best
estimate of climate
sensitivity close to 3 °C for doubled CO2 has been inferred from
paleoclimate data [51]--[52].
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 events.
Additionally, the GWPF report uses 68 percent confidence ranges throughout, so the 2.2 and 4.8 °C PALEOSENS
paleoclimate estimate is inconsistent with the GWPF low
sensitivity conclusions.
Various
paleoclimate - based equilibrium climate
sensitivity estimates from a range of geologic time periods.
In summary,
paleoclimate studies provide one line of evidence that supports an equilibrium climate
sensitivity between about 2 and 4.5 °C, and the GWPF justification for dismissing these
estimates is weak.
Instead, the report argues that this approach provides the only reliable method for
estimating climate
sensitivity, and that all other methods that produce higher
estimates (e.g.
paleoclimate and GCMs) are wrong.
These uncertainties may partly explain the typically weak correlations found between
paleoclimate indices and climate projections, and the difficulty in narrowing the spread in models» climate
sensitivity estimates from
paleoclimate - based emergent constraints (Schmidt et.
However, as Hansen notes, empirical
estimates of climate
sensitivity based on
paleoclimate data are consistent with the
sensitivity in climate models of approximately 3 °C for doubled atmospheric CO2.
In this manner, Hansen and Sato use climate models to help them
estimate past radiative forcings and surface temperature changes using
paleoclimate data without influencing their climate
sensitivity estimates.
To the authors,
sensitivity estimates based on
paleoclimate are worthy of discussion and
estimates based on GCMs are worthy of discussion, but
estimates based on actual observations are giving a throw away line.
You can not
estimate CO2
sensitivity in the ice ages or in the
paleoclimate without having good Albedo
estimates.
Efforts to
estimate climate
sensitivity from
paleoclimate records... face the additional challenge of a proxy record that contains major uncertainty.
Pekka,
paleoclimate being independent of models is valuable as another line of evidence, and in recent years the last 60 million years has become better constrained in temperature and CO2 to allow for
sensitivity ranges to be independently
estimated from it, as Hansen has done.