The DOI matches its Crossref record; 196 of the 196 references it cites were found in a registry or an index.
Information from Paleoclimate Archives
Abstract
Executive Summary Greenhouse-Gas Variations and Past Climate Responses It is a fact that present-day (2011) concentrations of the atmospheric greenhouse gases (GHGs) carbon dioxide (CO 2 ), methane (CH 4 ) and nitrous oxide (N 2 O) exceed the range of concentrations recorded in ice cores during the past 800,000 years . Past changes in atmospheric GHG concentrations can be determined with very high confidence from polar ice cores. Since AR4 these records have been extended from 650,000 years to 800,000 years ago. {5.2.2} With very high confidence , the current rates of CO 2 , CH 4 and N 2 O rise in atmospheric concentrations and the associated radiative forcing are unprecedented with respect to the highest resolution ice core records of the last 22,000 years . There is medium confidence that the rate of change of the observed GHG rise is also unprecedented compared with the lower resolution records of the past 800,000 years. {5.2.2} There is high confidence that changes in atmospheric CO 2 concentration play an important role in glacial–interglacial cycles . Although the primary driver of glacial–interglacial cycles lies in the seasonal and latitudinal distribution of incoming solar energy driven by changes in the geometry of the Earth's orbit around the Sun (“orbital forcing”), reconstructions and simulations together show that the full magnitude of glacial–interglacial temperature and ice volume changes cannot be explained without accounting for changes in atmospheric CO 2 content and the associated climate feedbacks. During the last deglaciation, it is very likely that global mean temperature increased by 3°C to 8°C.
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Cites
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The trajectory of the Anthropocene: The Great Acceleration
Steffen, W., Broadgate, W., Deutsch, L., Gaffney, O., & Ludwig, C. (2015) · The Anthropocene Review · doi:10.1177/2053019614564785 · Cited by 3,935
Glacial cooling and climate sensitivity revisited
Tierney, J. E., Zhu, J., King, J., Malevich, S. B., Hakim, G. J., & Poulsen, C. J. (2020) · Nature · doi:10.1038/s41586-020-2617-x · Cited by 573
Le Quéré, C., Peters, G. P., Andres, R. J., Andrew, R. M., Boden, T. A., Ciais, P., Friedlingstein, P., Houghton, R. A., Marland, G., Moriarty, R., et al. (2014) · Earth System Science Data · doi:10.5194/essd-6-235-2014 · Cited by 450
(2023) · Climate Change 2021 – The Physical Science Basis · doi:10.1017/9781009157896.003 · Cited by 298
Anchukaitis, K. J., Wilson, R., Briffa, K. R., Büntgen, U., Cook, E. R., D'Arrigo, R., Davi, N., Esper, J., Frank, D., Gunnarson, B. E., et al. (2017) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2017.02.020 · Cited by 294
Metadata
- Venue
- Climate Change 2013 – The Physical Science Basis
- Publisher
- Cambridge University Press
- Published
- 2014-03-24
- Pages
- 383-464
- OpenAlex
- W2255080690
- Cited by
- 481
- References
- 196
- FWCI
- 137.22
- Type
- book chapter
- Language
- en
- Open access
- closed
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