Climate sensitivity, sea level and atmospheric carbon dioxide
Open accessAbstract
Cenozoic temperature, sea level and CO 2 covariations 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 palaeoclimate data. Pleistocene climate oscillations yield a fast-feedback climate sensitivity of 3±1 ° C for a 4 W m −2 CO 2 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 ° C for a 4 W m −2 CO 2 forcing. Slow feedbacks, especially change of ice sheet size and atmospheric CO 2 , amplify the total Earth system sensitivity by an amount that depends on the time scale considered. Ice sheet response time is poorly defined, but we show that the slow response and hysteresis in prevailing ice sheet models are exaggerated. We use a global model, simplified to essential processes, to investigate state dependence of climate sensitivity, finding an increased sensitivity towards warmer climates, as low cloud cover is diminished and increased water vapour elevates the tropopause. Burning all fossil fuels, we conclude, would make most of the planet uninhabitable by humans, thus calling into question strategies that emphasize adaptation to climate change.
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Over the last ∼50 million years, global average surface temperatures steadily decreased from nearly 30°C during the early Eocene to less than 10°C during the most recent Pleistocene glacial epoch.
“For example, over the last ∼50 million years, global average surface temperatures have steadily decreased from nearly 30°C during the early Eocene (Burke et al. 2018, Hansen et al. 2013) to less than 10°C during the most recent Pleistocene glacial epoch (e.g., Tierney et al. 2020).”
From The History of Ocean Oxygenation (2022) · cites this paper as Hansen et al. 2013
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- Authors
- Hansen, J., Sato, M., Russell, G., & Kharecha, P.
- Affiliations
- Columbia University (US)
- Goddard Institute for Space Studies (US)
- Corresponding author
- Hansen, James
- Venue
- Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
- Publisher
- The Royal Society
- Published
- 2013-10-28
- Volume
- 371
- Issue
- 2001
- Pages
- 20120294
- ISSN
- 1364-503X (ISSN-L)
- 1471-2962
- PMC
- PMC3785813
- OpenAlex
- W2143037254
- Cited by
- 660
- References
- 154
- Citations by year
- 2026: 17 · 2025: 57 · 2024: 62 · 2023: 71 · 2022: 74 · 2021: 67 · 2020: 80 · 2019: 58 · 2018: 45 · 2017: 42 · 2016: 43 · 2015: 20 · 2014: 17 · 2013: 7
- FWCI
- 18.90
- Type
- journal article
- Language
- en
- Open access
- hybrid
- doi.org
- Locations
- Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences (publishedVersion, cc-by)
- Europe PMC (PubMed Central) (publishedVersion, cc-by)
- PubMed Central (publishedVersion, cc-by)
- PubMed (publishedVersion)
- arXiv (Cornell University) (submittedVersion)
- NASA STI Repository (National Aeronautics and Space Administration) (submittedVersion)
- arXiv (Cornell University)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate Change and Environmental Impact
- Keywords
- climate sensitivity, atmospheric CO2, Cenozoic climate, Pleistocene climate oscillations, Last Glacial Maximum, Holocene warming, Eemian interglacial, ice sheet response, low cloud cover, water vapor, tropopause, fossil fuel combustion, habitability
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