Sensitivity analysis of aerosol direct radiative forcing in ultraviolet—visible wavelengths and consequences for the heat budget

References

• Boucher, O. and Anderson, T. L. 1995. General circulation model assessment of the sensitivity of direct climate forcing by anthropogenic sulfate aerosols to aerosol size and chemistry. J. Geophys. Res. 100, 26 117-26 134.
   Google Scholar
• Box, M. A. and Trautmann, T. 1994. Computation of anthropogenic sulphate aerosol forcing using radiative perturbation theory. Tellus 46B, 33–39.
   Google Scholar
• Charlson, R. J., Langner, J., Rodhe, H., Leovt, C. and Warren, S. 1991. Perturbation of the northern hemisphere radiative balance by backscattering from anthropogenic sulfate aerosols. Tellus 43AB, 152–163
   Google Scholar
• Charlson, R. J., Lovelock, J. E., Andreae, M. and Warren, S. G. 1987. Oceanic phytoplankton, atmospheric sulphur, cloud albedo and climate. Nature 326, 655–661.
   Web of Science ®Google Scholar
• Charlson, R. J., Schwartz, S. E., Hales, J. M., Cess, R. D., Coakley, J. A., Jr, et al. 1992. Climate forcing by anthropogenic aerosols. Science 255,423–430.
   PubMed Web of Science ®Google Scholar
• D'Almeida, G. A., Koepke, P. and Shettle, E. P. 1991. Atmospheric Aerosols: Global Climatology and Radiative Characteristics. A. Deepak Publishing, Hampton, VA.
   Google Scholar
• Flossmann, A. I. 1998. Interaction of aerosol particles and clouds. J. Atmos. Sci. 55, 879–887.
   Web of Science ®Google Scholar
• Hansen, J., Sato, M. and Ruedy, R. 1997. Radiative forcing and climate response. J. Geophys. Res. 102,6831–6864.
   Web of Science ®Google Scholar
• Harvey, L. D. D. 2000. Constraining the aerosol radiative forcing and climate sensitivity. An editorial comment. Clim. Change. 44,413–418.
   Web of Science ®Google Scholar
• Hatzianastassiou, N., Katsoulis, B. and Vardavas, I. 2004. Global distribution of aerosol direct radiative forcing in the ultraviolet and visible arising under clear skies. Tellus B 56B, 51–71.
   Google Scholar
• Haywood, J. M. and Ramaswamy, V. 1998. Global sensitivity studies of the direct radiative forcing due to anthropogenic sulfate and black carbon aerosols. J. Geophys. Res. 103, 6043–6058.
   Web of Science ®Google Scholar
• Haywood, J. M., Ramaswamy, V. and Soden, B. J. 1998. Tropospheric aerosol climate forcing in clear-sky satellite observations over the oceans. Science 283, 1299–1303.
   Web of Science ®Google Scholar
• Haywood, J. M., Roberts, D. L., Slingo, A., Edwards, J. M. and Shine, K. P. 1997. General circulation model calculations of the direct radiative forcing by anthropogenic sulfate and fossil-fuel soot aerosol. J. Climate 10, 1562–1567.
   Web of Science ®Google Scholar
• Haywood, J. M. and Shine, K. P. 1997. Multi-spectral calculations of the direct radiative forcing by anthropogenic sulfate and fossil-fuel soot aerosols. Q. J. R. MeteoroL Soc. 123, 1907–1930.
   Web of Science ®Google Scholar
• Intergovernmental Panel on Climate Change (IPCC) 2001. Climate Change 2001: The Scientific Basis (eds. J. T. Houghton et al.). Cambridge University Press, New York.
   Google Scholar
• Jacobson, M. Z. 2001. Global direct radiative forcing due to multicomponent anthropogenic and natural aerosols. J. Geophys. Res. 106, 1551–1568.
   Web of Science ®Google Scholar
• Joseph, J. H., Wiscombe, W. J. and Weinmann, J. A. 1976. The delta-Eddington approximation of radiative flux transfer. J. Atmos. Sci. 33, 2452–2459.
   Web of Science ®Google Scholar
• Kaufman, Y. J., Tanre, D. and Boucher, O. 2002. A satellite view of aerosols in the climate system. Nature 419, 215–223.
   PubMed Web of Science ®Google Scholar
• Kay, M. J. and Box, M. 2000. Radiative effects of absorbing aerosols and impact of water vapor. J. Geophys. Res. 105, 12 221-12 234.
   Google Scholar
• Kiehl, J. T. and Briegleb, B. P. 1993. The relative roles of sulfate aerosols and greenhouse gases in climate forcing. Science 260, 311–314.
   PubMed Web of Science ®Google Scholar
• Koepke, P. and Hess, M. 1988. Scattering functions of tropospheric aerosols: the effect of nonspherical particles. Appl Opt. 27, 2422–2430.
   Web of Science ®Google Scholar
• Koepke, R, Hess, M., Schuh, I. and Shettle, E. P. 1997. Global Aerosol Data Set, Report no 243, Max-Planck Institut fiir Meteorologie, Hamburg. (Data available at http://www.meteo.physilc.uni-muenchen.de/strahlung/aerosol/aerosol.htm).
   Google Scholar
• Kondratyev, K. Y. 1999. Climatic effects of aerosols and clouds. Springer, New York.
   Google Scholar
• Lelieveld, L. and co-authors, 2002. Global air pollution crossroads over the Mediterranean. Science 298, 794–799.
   Google Scholar
• Myhre, G., Stordal, E, Restad, K. and Isaksen, I. S. A. 1998. Estimation of the direct radiative forcing due to sulfate and soot aerosols. Tellus 50B, 463–477.
   Google Scholar
• Nemesure, S., Wagener, R. and Schwartz, S. E. 1995. Direct short-wave forcing of climate by anthropogenic sulfate aerosol: sensitivity to particle size, composition, and relative humidity. J. Geophys. Res. 100, 26 105-26 116.
   Google Scholar
• Penner, J. E., Charslon, R. J., Hales, J. M., Laulainen, N. S., Leifer, R., et al. 1994. Quantifying and minimizing uncertainty of climate forcing by anthropogenic aerosols. Bull. Am. Meteorol Soc. 75, 375–400.
   Google Scholar
• Penner, J. E., Chuang, C. C. and Grant, K. 1998. Climate forcing by carbonaceous and sulfate aerosols. Climate Dyn. 14, 839–851.
   Web of Science ®Google Scholar
• Pilinis, Ch., Pandis, S. N. and Seinfeld, J. H. 1996. Sensitivity of direct climate forcing by anthropogenic aerosols to aerosol size distribution and composition. J. Geophys. Res. 100, 18 739-18 754.
   Google Scholar
• Pruppacher, H. R. and Klett, J. D. 1997. Microphysics of Clouds and Precipitation, 2nd revised and enlarged edition. Kluwer Academic Publishers, Dordrecht.
   Google Scholar
• Ramanathan, V., Crutzen, P. J., Kiehl, J. T. and Rosenfeld, D. 2001. Aerosols, climate, and the hydrological cycle. Science 294, 2119–2124.
   Google Scholar
• Rossow, W. B. and Schiffer, R. A. 1999. Advances in understanding clouds from ISCCP. Bull. Am. Meteorol Soc. 80, 2261–2287.
   Web of Science ®Google Scholar
• Satheesh, S. K. and Ramanathan, V. 2000. Large differences in tropical aerosol forcing at the top of the atmosphere and Earth's surface. Nature 405, 60–63.
   PubMed Web of Science ®Google Scholar
• Schult, I., Feichter, J. and Cooke, W. F. 1997. Effect of black carbon and sulfate aerosols on the global radiation budget. J. Geophys. Res. 102, 30 107-30 117.
   Google Scholar
• Shettle, E. P. and Fenn, R. W. 1979. Models for the aerosols of the lower atmosphere and the effects of humidity variations on their op-tical properties, AFGL-TR-79-0214, Environmental Research Paper no 675, U.S. Air Force Geophysics Laboratory, Hanscom Air Force Base, Mass.
   Google Scholar
• Shettle, E. P. and Weinmann, J. A. 1970. The transfer of solar irradiance through inhomogeneous turbid atmospheres evaluated by Eddington's approximation. J. Atmos. Sci. 27, 1048–1055.
   Web of Science ®Google Scholar
• Sinha, A. and Harries, J. E. 1997. Possible change in climate param-eters with zero net radiative forcing. Geophys. Res. Lett. 24, 2335–2358.
   Web of Science ®Google Scholar
• Tegen, I., Koch, D., Lads, A. A. and Sato, M. 2000. Trends in tropo-spheric aerosol loads and corresponding impact on direct radiative forcing between 1950 and 1990: a model study. J. Geophys. Res. 105, 26 971-26 989.
   Google Scholar
• Wendisch, M., Heintzenberg, J. and Bussemer, M. 2001. Measurement-based aerosol forcing calculations: the influence of model complexity. Meteorol Z. 10, 45–60.
   Web of Science ®Google Scholar
• West, J. J., Pilinis, C., Nenes, A. and Pandis, S. N. 1998. Marginal direct climate forcing by atmospheric aerosols. Atmos. Environ. 32, 2531–2542.
   Google Scholar