Paleoclimate Implications for Human-Made Climate Change

By J. Hansen, Makiko Sato. 2011

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Paleoclimate data help us assess climate sensitivity and potential human-made climate effects. We conclude that Earth in the warmest interglacial periods of the past million years was less than 1°C warmer than in the Holocene. Polar warmth in these interglacials and in the Pliocene does not imply that a substantial cushion remains between today’s climate and dangerous warming, but rather that Earth is poised to experience strong amplifying polar feedbacks in response to moderate global warming. Thus, goals to limit human-made warming to 2°C are not sufficient—they are prescriptions for disaster. Ice sheet disintegration is nonlinear, spurred by amplifying feedbacks. We suggest that ice sheet mass loss, if warming continues unabated, will be characterized better by a doubling time for mass loss rate than by a linear trend. Satellite gravity data, though too brief to be conclusive, are consistent with a doubling time of 10 years or less, implying the possibility of multimeter sea level rise this century. Observed accelerating ice sheet mass loss supports our conclusion that Earth’s temperature now exceeds the mean Holocene value. Rapid reduction of fossil fuel emissions is required for humanity to succeed in preserving a planet resembling the one on which civilization developed.

Subfields: Atmospheric Science, Oceanography

View Paper: https://www.semanticscholar.org/paper/9d21cc211caff587de804cadbd9e399fa91d43e0

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Citations in the corpus

Earth's energy imbalance and implications (2011, background): “The equilibrium climate sensitivity of most models is within or near the range 3 ± 0.5 C for doubled CO 2 dictated by paleoclimate data (Hansen and Sato, 2012).”