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Global estimate of aerosol direct radiative forcing from satellite measurements

Abstract

Atmospheric aerosols cause scattering and absorption of incoming solar radiation. Additional anthropogenic aerosols released into the atmosphere thus exert a direct radiative forcing on the climate system1. The degree of present-day aerosol forcing is estimated from global models that incorporate a representation of the aerosol cycles1,2,3. Although the models are compared and validated against observations, these estimates remain uncertain. Previous satellite measurements of the direct effect of aerosols contained limited information about aerosol type, and were confined to oceans only4,5. Here we use state-of-the-art satellite-based measurements of aerosols6,7,8 and surface wind speed9 to estimate the clear-sky direct radiative forcing for 2002, incorporating measurements over land and ocean. We use a Monte Carlo approach to account for uncertainties in aerosol measurements and in the algorithm used. Probability density functions obtained for the direct radiative forcing at the top of the atmosphere give a clear-sky, global, annual average of -1.9 W m-2 with standard deviation, ± 0.3 W m-2. These results suggest that present-day direct radiative forcing is stronger than present model estimates, implying future atmospheric warming greater than is presently predicted, as aerosol emissions continue to decline10.

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Figure 1: In situ observations of the AMF.
Figure 2: Anthropogenic AOT at 0.55 µm.
Figure 3: PDFs of the clear-sky shortwave aerosol DRF on an annual, global average.

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References

  1. Ramaswamy, V. et al. (ed.) Climate Change 2001: The Scientific Basis. Contribution of WGI to the Third Assessment Report of the IPCC (Cambridge Univ., Cambridge, 2001)

  2. Reddy, M. S. et al. Estimates of global multi-component aerosol optical depth and direct radiative perturbation in the LMDZT General Circulation Model. J. Geophys. Res. 110, doi:10.1029/2004JD004757 (2005)

  3. Roberts, D. L. & Jones, A. Climate sensitivity to black carbon aerosol from fossil fuel combustion. J. Geophys. Res. 109, doi:10.1029/2004JD004676 (2004)

  4. Bellouin, N., Boucher, O., Tanré, D. & Dubovik, O. Aerosol absorption over the clear-sky oceans deduced from POLDER-1 and AERONET observations. Geophys. Res. Lett. 30, doi:10.1029/2003GL017121 (2003)

  5. Christopher, S. A. & Zhang, J. Shortwave aerosol radiative forcing from MODIS and CERES observations over the oceans. Geophys. Res. Lett. 29, doi:10.1029/2002GL014803 (2002)

  6. Kaufman, Y. J. et al. Operational remote sensing of tropospheric aerosol over land from EOS moderate resolution imaging spectroradiometer. J. Geophys. Res. 102, 17051–17068 (1997)

    Article  ADS  CAS  Google Scholar 

  7. Tanré, D., Kaufman, Y. J., Herman, M. & Mattoo, S. Remote sensing of aerosol properties over oceans using the MODIS/EOS spectral radiances. J. Geophys. Res. 102, 16971–16988 (1997)

    Article  ADS  Google Scholar 

  8. Herman, J. R. et al. Global distribution of UV-absorbing aerosols from Nimbus 7/TOMS data. J. Geophys. Res. 102, 16911–16922 (1997)

    Article  ADS  CAS  Google Scholar 

  9. Wentz, F. A well calibrated ocean algorithm for SSM/I. J. Geophys. Res. 102, 8703–8718 (1997)

    Article  ADS  Google Scholar 

  10. Andreae, M. O., Jones, C. D. & Cox, P. M. Strong present-day aerosol cooling implies a hot future. Nature 435, 1187–1190 (2005)

    Article  ADS  CAS  Google Scholar 

  11. Osborne, S. R. & Haywood, J. M. Aircraft observations of the physical and optical properties of major aerosol types. Atmos. Res. 73, 173–201 (2005)

    Article  CAS  Google Scholar 

  12. Dubovik, O. et al. Variability of absorption and optical properties of key aerosol types observed in worldwide locations. J. Atmos. Sci. 59, 590–608 (2002)

    Article  ADS  Google Scholar 

  13. Takemura, T., Nozawa, T., Emori, S., Nakajima, T. Y. & Nakajima, T. Simulation of climate response to aerosol direct and indirect effects with aerosol transport-radiation model. J. Geophys. Res. 110, doi:10.1029/2004JD005029 (2005)

  14. Collins, W. D. et al. Simulation of aerosol distributions and radiative forcing for INDOEX: Regional climate impacts. J. Geophys. Res. 107, doi:10.1029/2000JD000032 (2002)

  15. Stier, P. et al. The aerosol-climate model ECHAM5-HAM. Atmos. Chem. Phys. 5, 1125–1156 (2005)

    Article  ADS  CAS  Google Scholar 

  16. Kirkevåg, A. & Iversen, T. Global direct radiative forcing by process-parameterized aerosol optical properties. J. Geophys. Res. 107, doi:10.1029/2001JD000886 (2002)

  17. Platnick, S. et al. The MODIS cloud products: algorithms and examples from Terra. IEEE Trans. Geosci. Remote Sens. 41, 459–473 (2003)

    Article  ADS  Google Scholar 

  18. Keil, A. & Haywood, J. M. Solar radiative forcing by biomass aerosol particles over marine clouds during SAFARI-2000. J. Geophys. Res. 108, doi:10.1029/2002JD002315 (2003)

  19. Remer, L. A. et al. The MODIS aerosol algorithm, products, and validation. J. Atmos. Sci. 62, 947–973 (2005)

    Article  ADS  Google Scholar 

  20. Smirnov, A., Holben, B. N., Eck, T. F., Dubovik, O. & Slutsker, I. Effect of wind speed on columnar aerosol optical properties at Midway Island. J. Geophys. Res. 108, doi:10.1029/2003JD003879 (2003)

  21. Cox, C. & Munk, W. Statistics of the sea surface derived from sun glitter. J. Mar. Res. 13, 198–227 (1954)

    Google Scholar 

  22. Schaaf, C. B. et al. First operational BRDF, albedo nadir reflectance products from MODIS. Remote Sens. Environ. 83, 135–148 (2002)

    Article  ADS  Google Scholar 

  23. Key, J. R. & Schweiger, A. J. Tools for atmospheric radiative transfer: STREAMER and FLUXNET. Comput. Geosci. 24, 443–451 (1998)

    Article  ADS  Google Scholar 

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Acknowledgements

The work by N.B., O.B. and J.H. was supported by the UK Department for Environment, Food and Rural Affairs under the Climate Prediction Programme. We thank B. Crouzille for helping with the processing of MODIS data. M. Schulz and the AEROCOM participants are thanked for their efforts and for letting us use their data. Author Contributions All authors contributed equally to this work.

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Correspondence to Nicolas Bellouin.

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Bellouin, N., Boucher, O., Haywood, J. et al. Global estimate of aerosol direct radiative forcing from satellite measurements. Nature 438, 1138–1141 (2005). https://doi.org/10.1038/nature04348

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