Skip to main content
Log in

Simulation of the radiative effect of black carbon aerosols and the regional climate responses over China

  • Published:
Advances in Atmospheric Sciences Aims and scope Submit manuscript

Abstract

As part of the development work of the Chinese new regional climate model (RIEMS), the radiative process of black carbon (BC) aerosols has been introduced into the original radiative procedures of RIEMS, and the transport model of BC aerosols has also been established and combined with the RIEMS model. Using the new model system, the distribution of black carbon aerosols and their radiative effect over the China region are investigated. The influences of BC aerosole on the atmospheric radiative transfer and on the air temperature, land surface temperature, and total rainfall are analyzed. It is found that BC aerosols induce a positive radiative forcing at the top of the atmosphere (TOA), which is dominated by shortwave radiative forcing. The maximum radiative forcing occurs in North China in July and in South China in April. At the same time, negative radiative forcing is observed on the surface. Based on the radiative forcing comparison between clear sky and cloudy sky, it is found that cloud can enforce the TOA positive radiative forcing and decrease the negative surface radiative forcing. The responses of the climate system in July to the radiative forcing due to BC aerosols are the decrease in the air temperature in the middle and lower reaches of the Changjiang River and Huaihe area and most areas of South China, and the weak increase or decrease in air temperature over North China. The total rainfall in the middle and lower reaches of the Changjiang River area is increased, but it decreased in North China in July.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Chen Longxun., Shao Yongning, Zhang Qingfen, and Ren Zhenhai, 1991: Preliminary analysis of climate change during the last 39 years in China.Quarterly Journal of Applied Meteorology,2, 164–174. (in Chinese)

    Google Scholar 

  • D’ Almeida, G. A., P. Koepke, and E. P. Shettle, Eds., 1991:Global Climatology and Radiative Characteristics. Vol.126,Atmospheric Aerosols, A Deepak Publishing, Hampton, Virginia, 561pp.

  • Grant, K. E., C. C. Chuang, A. S. Grossman, and J. E. Penner, 1999: Modeling the spectral optic properties of ammonium sulfate and biomass aerosols: Parameterization of relative humidity effects and model results.Atmos. Environ.,33, 2603–2620.

    Article  Google Scholar 

  • Hansen, J., Mki. Sato, and R. Ruedy, 1997: Radiative forcing and climate response.J. Geophys. Res.,102, 6831–6864.

    Article  Google Scholar 

  • Hansen, J., Mki. Sato, R. Ruedy, A. Lacis, and V. Oinas, 2000: Global warming in the twenty-first century: An alternative scenario.Proc. Natl. Acad. Sci., U.S.A.,97, 9875–9880.

    Article  Google Scholar 

  • Haywood, J., and V. Ramaswamy, 1998: Global sensitivity studies of the direct radiative forcing due to anthropogenic sulphate and black carbon aerosols.J. Geophys. Res.,103, 6043–6058.

    Article  Google Scholar 

  • Haywood, J. M., D. L. Roberts, A. Slingo, J. M. Edwards, and K. P. Shine, 1997: General circulation model calculations of the direct radiative forcing by anthropogenic sulfate and fossil-fuel soot aerosol.J. Climate,10, 1562–1577.

    Article  Google Scholar 

  • Jacobson, M. Z., 2000: A physically-based treatment of elemental carbon optics: Implications for global direct forcing of aerosols.Geophys. Res. Lett.,27, 217–220.

    Article  Google Scholar 

  • Jacobson, M. Z., 2001: Global direct radiative forcing due to multicomponent anthropogenic and natural aerosols.J. Geophys. Res.,106, 1551–1568.

    Article  Google Scholar 

  • Liousse, C., J. E. Penner, C. C. Chuang, J. J. Walton, and H. Eddleman, 1996: A global three dimensional model study of carbonaceous aerosols.J. Geophys. Res.,101, 19411–19432.

    Article  Google Scholar 

  • Martins, J. V., P. Artaxo, C. Liousse, J. S. Reid, P. V. Hobbs, and Y. J. Kaufman, 1998: Effects of black carbon content, particle size, and aerosols, their direct and indirect effects mixing on light absorption by aerosols from biomass burning in Brazil.J. Geophys. Res.,103, 32041–32050.

    Article  Google Scholar 

  • Menon, S., J. Hansen, L. Nazarenko, and Y. Luo, 2002: Climate effects of black carbon aerosols in China and India.Science,297, 2250–2253.

    Article  Google Scholar 

  • Schult, I., J. Feichter, and W. F. Cooke, 1997: Effect of black carbon and sulphate aerosols on the global radiation budget.J. Geophys. Res.,102, 30107–30117.

    Article  Google Scholar 

  • Streets, D. G., and Coauthors, 2003: An inventory of gaseous and primary aerosol emissions in Asia in the year 2000.J. Geophys. Res.,108(D21), 8809, doi10. 1029/2002JD003093.

    Article  Google Scholar 

  • Tang Jie, Wen Yupu, Zhou Lingxi, Qi Donglin, Zheng Ming, T. Neil, and W. Erika, 1999: Observational study of black carbon in clean air area of western China.Quarterly Journal of Applied Meteorology,10, 160–169. (in Chinese)

    Google Scholar 

  • Wang Mingxing, Zhang Renjian, and Pu Yifen, 2001: Recent researches on aerosol in China.Adv. Atmos. Sci.,18, 576–586.

    Article  Google Scholar 

  • Wang Xihong, and Shi Guangyu, 2002: Effect of cloud and surface albedo on direct sulfate radiative forcing over East Asia.Acta Meteorologica Sinica,60, 758–764. (in Chinese)

    Google Scholar 

  • William, F. C., and J. J. N. Wilson, 1996: A global carbon aerosol model.J. Geophys. Res.,101, 19395–19409.

    Article  Google Scholar 

  • Wolf, M. E., and G. M. Hidy, 1997: Aerosols and climate: Anthropogenic emissions and trends for 50 years.J. Geophys. Res.,102, 11113–11121.

    Article  Google Scholar 

  • Wu Jian, Jiang Weimei, Liu Hongnian, and Tang Jianping, 2002: Simulation of the direct and indirect radiative effects of sulfate aerosol.Acta Scientiae Circumstantiae,22, 129–134. (in Chinese)

    Google Scholar 

  • Xiong Zhe, 2001: The simulation and analysis of East Asia climate and its interannual variation. Ph. D. Dissertation, Institute of Atmospheric Physics, Chinese Academy of Sciences, 185pp.

  • Zhang Lisheng, and Shi Guangyu, 2000: The global anthropogenic sulfate and soot data and distribution characteristic of the optical depth.Climatic and Environmental Research,5, 67–74. (in Chinese)

    Google Scholar 

  • Zhang Lisheng, and Shi Guangyu, 2001: The simulation and estimation of radiative properties and radiative forcing due to sulfate and soot aerosols.Chinese Journal of Atmospheric Sciences,25, 231–242. (in Chinese)

    Google Scholar 

  • Zhang Ying, and Gao Qinxian, 1997: A study on the radiative effect of sulfate and soot aerosols.Quarterly Journal of Applied Meteorology,8(Suppl.), 87–91. (in Chinese)

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Wu Jian.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Wu, J., Jiang, W., Fu, C. et al. Simulation of the radiative effect of black carbon aerosols and the regional climate responses over China. Adv. Atmos. Sci. 21, 637–649 (2004). https://doi.org/10.1007/BF02915731

Download citation

  • Received:

  • Revised:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02915731

Key words

Navigation