Abstract
Under present growth rates of greenhouse gas and black carbon aerosol emissions, global mean temperatures can warm by as much as 2 °C from pre-industrial temperatures by about 20501,2. Mitigation of the four short-lived climate pollutants (SLCPs), methane, tropospheric ozone, hydrofluorocarbons and black carbon, has been shown to reduce the warming trend by about 50% (refs 1, 2) by 2050. Here we focus on the potential impact of this SLCP mitigation on global sea-level rise (SLR). The temperature projections under various SLCP scenarios simulated by an energy-balance climate model1 are integrated with a semi-empirical SLR model3, derived from past trends in temperatures and SLR, to simulate future trends in SLR. A coupled ocean–atmosphere climate model4 is also used to estimate SLR trends due to just the ocean thermal expansion. Our results show that SLCP mitigation can have significant effects on SLR. It can decrease the SLR rate by 24–50% and reduce the cumulative SLR by 22–42% by 2100. If the SLCP mitigation is delayed by 25 years, the warming from pre-industrial temperature exceeds 2 °C by 2050 and the impact of mitigation actions on SLR is reduced by about a third.
This is a preview of subscription content, access via your institution
Relevant articles
Open Access articles citing this article.
-
Path to net zero is critical to climate outcome
Scientific Reports Open Access 12 November 2021
-
Emergency deployment of direct air capture as a response to the climate crisis
Nature Communications Open Access 14 January 2021
-
Impact of methane and black carbon mitigation on forcing and temperature: a multi-model scenario analysis
Climatic Change Open Access 17 September 2020
Access options
Subscribe to this journal
Receive 12 print issues and online access
$209.00 per year
only $17.42 per issue
Rent or buy this article
Prices vary by article type
from$1.95
to$39.95
Prices may be subject to local taxes which are calculated during checkout


References
Ramanathan, V. & Xu, Y. The Copenhagen Accord for limiting global warming: Criteria, constraints, and available avenues. Proc. Natl Acad. Sci. USA 107, 8055–8062 (2010).
Integrated Assessment of Black Carbon and Tropospheric Ozone (UNEP & WMO, 2011).
Vermeer, M. & Rahmstorf, S. Global sea level linked to global temperature. Proc. Natl Acad. Sci. USA 106, 21527–21532 (2009).
Gent, P. R. et al. The community climate system model version 4. J. Clim. 24, 4973–4991 (2011).
Forster, P. et al. in IPCC Climate Change 2007: The Physical Science Basis (eds Solomon, S. et al.) Ch. 2 (Cambridge Univ. Press, 2007).
Meehl, G. A. et al. in IPCC Climate Change 2007: The Physical Science Basis (eds Solomon, S. et al.) Ch. 10 (Cambridge Univ. Press, 2007).
Ramanathan, V. & Feng, Y. On avoiding dangerous anthropogenic interference with the climate system: Formidable challenges ahead. Proc. Natl Acad. Sci. USA 105, 14245–14250 (2008).
Levitus, S. et al. World ocean heat content and thermosteric sea level change (0–2000 m), 1955–2010. Geophys. Res. Lett. 39, 1–5 (2012).
Gleckler, P. J. et al. Human-induced global ocean warming on multidecadal timescales. Nature Clim. Change 2, 524–529 10.1038/nclimate1553(2012).
Nakićenović, N. & Swart, R. (eds) IPCC Special Report on Emissions Scenarios (Cambridge Univ. Press, 2000).
Wallack, J. & Ramanthan, V. The other climate changers—Why black carbon and ozone also matter. Foreign Aff. 88, 105–113 (2009).
Molina, M. et al. Reducing abrupt climate change risk using the Montreal Protocol and other regulatory actions to complement cuts in CO2 emissions. Proc. Natl Acad. Sci. USA 106, 20616–20621 (2009).
Shindell, D. et al. Simultaneously mitigating near-term climate change and improving human health and food security. Science 335, 183–187 (2012).
Meehl, G. A. et al. Relative outcomes of climate change mitigation related to global temperature versus sea level rise. Nature Clim. Change 2, 576–580 (2012).
Peltier, W. R. Closure of the budget of global sea level rise over the GRACE era: The importance and magnitudes of the required corrections for global glacial isostatic adjustment. Quat. Sci. Rev. 28, 1658–1674 (2009).
Church, J. A. et al. Revisiting the Earth’s sea level and energy budgets from 1961 to 2008. Geophys. Res. Lett. 38, L18601 (2011).
Jacob, T. et al. Recent contributions of glaciers and ice caps to sea level rise. Nature 482, 514–518 (2012).
Stepherd, A. et al. A reconciled estimate of ice-sheet mass balance. Science 338, 1183–1189 (2012).
Hansen, J. et al. Global surface temperature change. Rev. Geophys. 48, 1–29 (2010).
Church, J. A. & White, N. J. A 20th-century acceleration in global sea-level rise. Geophys. Res. Lett. 33, L01602 (2006).
Cofala, J., Amann, M., Klimont, Z., Kupiainen, K. & Hoglund-Isaksson, L. Scenarios of global anthropogenic emissions of air pollutants and methane until 2030. Atmos Environ. 41, 8486–8499 (2007).
Church, J. A. & White, N. J. Sea-level rise from the late 19th to the early 21st century. Surv. Geophys. 32, 585–602 (2011).
Rahmstorf, S., Perrette, M. M. & Vermeer, M. Testing the robustness of semi-empirical sea level projections. Clim. Dyn. 39, 861–875 (2011).
Solomon, S., Plattner, G-K., Knutti, R. & Friedlingstein, P. Irreversible climate change due to carbon dioxide emissions. Proc. Natl Acad. Sci. USA 106, 1704–1709 (2009).
Friedlingstein, P. Long-term climate implications of twenty-first century options for carbon dioxide emission mitigation. Nature Clim. Change 1, 457–461 (2011).
Pardaens, A. K., Gregory, J. M. & Lowe, J. A. A model study of factors influencing projected changes in regional sea level over the twenty-first century. Clim. Dyn. 36, 2015–2033 (2011).
Yin, J. Century to multi-century sea level rise projections from CMIP5 models. Geophys. Res. Lett. 39, L17709 10.1029/2012GL052947(2012).
Hu, A., Meehl, G. A., Han, W. & Yin, J. Effect of the potential melting of the Greenland ice sheet on the meridional overturning circulation and global climate in the future. Deep Sea Res. II 58, 1914–1926 (2011).
Mitrovica, J. X., Tamisiea, M. E., Davis, J. L. & Milne, G. A. Recent mass balance of polar ice sheets inferred from patterns of global sea level change. Nature 409, 1026–1029 (2011).
Kopp, R. E. et al. The impact of Greenland melt on regional sea level: A partially coupled analysis of dynamic and static equilibrium effects in idealized water-hosing experiments. Climatic Change 103, 619–625 (2010).
Acknowledgements
This study was financially supported by the National Science Foundation (ATM07-21142). A portion of this study was also supported by the Office of Science (BER), US Department of Energy, Cooperative Agreement No. DE-FC02-97ER62402. The National Center for Atmospheric Research is funded by the National Science Foundation.
Author information
Authors and Affiliations
Contributions
V.R. designed and led the study, A.H., Y.X., C.T. and W.M.W. contributed to the model simulations and data analysis, and all authors actively contributed to writing the manuscript.
Corresponding author
Ethics declarations
Competing interests
The authors declare no competing financial interests.
Supplementary information
Supplementary Information
Supplementary Information (PDF 1319 kb)
Rights and permissions
About this article
Cite this article
Hu, A., Xu, Y., Tebaldi, C. et al. Mitigation of short-lived climate pollutants slows sea-level rise. Nature Clim Change 3, 730–734 (2013). https://doi.org/10.1038/nclimate1869
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1038/nclimate1869
This article is cited by
-
Development of waste-to-energy through integrated sustainable waste management: the case of ABREN WtERT Brazil towards changing status quo in Brazil
Waste Disposal & Sustainable Energy (2023)
-
Path to net zero is critical to climate outcome
Scientific Reports (2021)
-
Emergency deployment of direct air capture as a response to the climate crisis
Nature Communications (2021)
-
Climate co-benefits of air quality and clean energy policy in India
Nature Sustainability (2020)
-
Mitigating the impacts of air pollutants in Nepal and climate co-benefits: a scenario-based approach
Air Quality, Atmosphere & Health (2020)