Century-scale effects of increased atmospheric C02 on the ocean–atmosphere system
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The upper ocean becomes globally more stratified owing to increases in surface temperature and precipitation.
“Additionally, the upper ocean becomes globally more stratified owing to increases in surface temperature and precipitation [Manabe et al., 1991; Manabe and Stouffer, 1993; Sarmiento et al., 1998].”
From Potential impact of climate change on marine export production (2001) · cites this paper as Manabe and Stouffer, 1993
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Simulated response of the ocean carbon cycle to anthropogenic climate warming
Sarmiento, J. L., Hughes, T. M. C., Stouffer, R. J., & Manabe, S. (1998) · Nature · doi:10.1038/30455 · Cited by 899 · see citing works
Self-citationPotential impact of climate change on marine export production
Bopp, L., Monfray, P., Aumont, O., Dufresne, J., Le Treut, H., Madec, G., Terray, L., & Orr, J. C. (2001) · Global Biogeochemical Cycles · doi:10.1029/1999gb001256 · Cited by 514 · see citing works
Multiple timescales for neutralization of fossil fuel CO <sub>2</sub>
Archer, D., Kheshgi, H., & Maier‐Reimer, E. (1997) · Geophysical Research Letters · doi:10.1029/97gl00168 · Cited by 314 · see citing works
Dynamics of fossil fuel CO <sub>2</sub> neutralization by marine CaCO <sub>3</sub>
Archer, D., Kheshgi, H., & Maier‐Reimer, E. (1998) · Global Biogeochemical Cycles · doi:10.1029/98gb00744 · Cited by 274 · see citing works
Probabilistic climate change projections using neural networks
Knutti, R., Stocker, T. F., Joos, F., & Plattner, G.-K. (2003) · Climate Dynamics · doi:10.1007/s00382-003-0345-1 · Cited by 197 · see citing works
Improvement of CO2 uptake of activated carbons by treatment with mineral acids
Gęsikiewicz-Puchalska, A., Zgrzebnicki, M., Michalkiewicz, B., Narkiewicz, U., Morawski, A. W., & Wrobel, R. J. (2017) · Chemical Engineering Journal · doi:10.1016/j.cej.2016.10.005 · Cited by 66 · see citing works
Kularatne, K., Sissmann, O., Kohler, E., Chardin, M., Noirez, S., & Martinez, I. (2018) · Applied Geochemistry · doi:10.1016/j.apgeochem.2018.05.020 · Cited by 52 · see citing works
- Authors
- Manabe, S., & Stouffer, R. J.
- Affiliations
- NOAA Geophysical Fluid Dynamics Laboratory (US)
- ORCID
- Stouffer, Ronald J.
- Venue
- Nature
- Published
- 1993-07
- Volume
- 364
- Issue
- 6434
- Pages
- 215-218
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W1984177133
- Cited by
- 490
- References
- 0
- Citations by year
- 2026: 4 · 2025: 4 · 2024: 12 · 2023: 15 · 2022: 12 · 2021: 5 · 2020: 17 · 2019: 7 · 2018: 8 · 2017: 5 · 2016: 8 · 2015: 8 · 2014: 6 · 2013: 7 · 2012: 10
- FWCI
- 47.65
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature (publishedVersion)
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Keywords
- elevated CO2, ocean-atmosphere interaction, thermohaline circulation, ocean ventilation, sea level rise, thermal expansion, ice sheet melting, global mean temperature, carbon cycle, ocean biogeochemistry, climate change projections
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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