Climate Sensitivity, Sea Level, and Atmospheric CO2
James Hansen, Makiko Sato, Gary Russell, Pushker Kharecha (NASA, Goddard Institute for Space Studies, Columbia University Earth Institute)

TL;DR
This paper examines paleoclimate data to estimate climate sensitivity, highlighting the impact of feedback mechanisms, and warns that burning all fossil fuels could render much of Earth uninhabitable.
Contribution
It provides a refined estimate of climate sensitivity based on paleoclimate data and investigates the state-dependence of sensitivity through simplified global modeling.
Findings
Pleistocene data suggests a climate sensitivity of 3 +/- 1°C for 4 W/m2 CO2 forcing.
Glacial-interglacial transitions imply a sensitivity of 3-4°C for 4 W/m2 CO2.
Burning all fossil fuels could make large parts of Earth uninhabitable.
Abstract
Cenozoic temperature, sea level and CO2 co-variations provide insights into climate sensitivity to external forcings and sea level sensitivity to climate change. Climate sensitivity depends on the initial climate state, but potentially can be accurately inferred from precise paleoclimate data. Pleistocene climate oscillations yield a fast-feedback climate sensitivity 3 +/- 1{\deg}C for 4 W/m2 CO2 forcing if Holocene warming relative to the Last Glacial Maximum (LGM) is used as calibration, but the error (uncertainty) is substantial and partly subjective because of poorly defined LGM global temperature and possible human influences in the Holocene. Glacial-to-interglacial climate change leading to the prior (Eemian) interglacial is less ambiguous and implies a sensitivity in the upper part of the above range, i.e., 3-4{\deg}C for 4 W/m2 CO2 forcing. Slow feedbacks, especially change of…
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