Using the past to constrain the future: how the palaeorecord can improve estimates of global warming
Tamsin L. Edwards, Michel Crucifix, Sandy P. Harrison

TL;DR
This paper reviews how paleoclimate data can be utilized alongside instrumental records to better constrain estimates of climate sensitivity, aiming to reduce uncertainties in future climate change predictions.
Contribution
It highlights methods for integrating geological past climate data with modern observations to improve climate sensitivity estimates and discusses ways to enhance this approach.
Findings
Paleoclimate records can provide valuable constraints on climate sensitivity.
Current methods have limitations that can be addressed to improve accuracy.
Integrating geological data with instrumental records can reduce uncertainty in climate projections.
Abstract
Climate sensitivity is defined as the change in global mean equilibrium temperature after a doubling of atmospheric CO2 concentration and provides a simple measure of global warming. An early estimate of climate sensitivity, 1.5-4.5{\deg}C, has changed little subsequently, including the latest assessment by the Intergovernmental Panel on Climate Change. The persistence of such large uncertainties in this simple measure casts doubt on our understanding of the mechanisms of climate change and our ability to predict the response of the climate system to future perturbations. This has motivated continued attempts to constrain the range with climate data, alone or in conjunction with models. The majority of studies use data from the instrumental period (post-1850) but recent work has made use of information about the large climate changes experienced in the geological past. In this…
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