Skip to main content
Log in

Response of the East Asian summer monsoon to large volcanic eruptions during the last millennium

  • Article
  • Atmospheric Science
  • Published:
Chinese Science Bulletin

Abstract

The responses of the East Asian summer monsoon (EASM) to large volcanic eruptions were analyzed using a millennial simulation with the FGOALS-gl climate system model. The model was driven by both natural (solar irradiance, volcanic eruptions) and anthropogenic (greenhouse gases, sulfate aerosols) forcing agents. The results showed cooling anomalies after large volcanic eruptions almost on a global scale. The cooling over the continental region is stronger than that over the ocean. The precipitation generally decreases in the tropical and subtropical regions in the first summer after large volcanic eruptions. Cooling with amplitudes up to −0.3 °C is seen over eastern China in the first summer after large volcanic eruptions. The East Asian continent is dominated by northeasterly wind anomalies and the corresponding summer rainfall exhibits a coherent reduction over the whole of eastern China. An analysis of the surface heat flux suggested the reduction in summer precipitation over eastern China can be attributed to a decrease of moisture vapor over the tropical oceans, and the weakening of the EASM may be attributed to the reduced land–sea thermal contrast after large volcanic eruptions.

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.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5

Similar content being viewed by others

References

  1. Lamb HH (1970) Volcanic dust in the atmosphere, with a chronology and assessment of its meteorological significance. Philos Trans R Soc Ser A 266:425–533

    Article  Google Scholar 

  2. Cole-Dai J, Mosley-Thompson E, Thompson LG (1997) Annually resolved southern hemisphere volcanic history from two Antarctic ice cores. J Geophys Res 102:16761–16771

    Article  Google Scholar 

  3. Gao CC, Oman L, Robock A et al (2007) Atmospheric volcanic loading derived from bipolar ice cores: accounting for the spatial distribution of volcanic deposition. J Geophys Res 112:D09109

    Google Scholar 

  4. Crowley TJ (2000) Causes of climate change over the past 1000 years. Science 289:270–277

    Article  Google Scholar 

  5. Stowe L, Carey R, Pellegrino P (1992) Monitoring the Mt. Pinatubo aerosol layer with NOAA/11 AVHRR data. Geophys Res Lett 19:159–162

    Article  Google Scholar 

  6. Trepte CR, Veiga RE, McCormick MP (1993) The poleward dispersal of Mount Pinatubo volcanic aerosol. J Geophys Res 98:18563–18573

    Article  Google Scholar 

  7. Minnis P, Harrison EF, Stowe LL (1993) Radiative climate forcing by the Mount Pinatubo eruption. Science 259:1411–1415

    Article  Google Scholar 

  8. Robock A, Mao J (1992) Winter warming from large volcanic eruptions. Geophys Res Lett 19:2405–2408

    Article  Google Scholar 

  9. Allen MR, Ingram WJ (2002) Constraints on the future changes in climate and the hydrological cycle. Nature 419:224–232

    Article  Google Scholar 

  10. Gillett NP, Weaver AJ, Zwiers FW et al (2004) Detection of volcanic influence on global precipitation. Geophys Res Lett 31:L12217

    Article  Google Scholar 

  11. Lambert FH, Gillett NP, Stone DA et al (2005) Attribution studies of observed land precipitation changes with nine coupled models. Geophys Res Lett 32:L18704

    Article  Google Scholar 

  12. Trenberth KE, Dai AG (2007) Effects of Mount Pinatubo volcanic eruption on the hydrological cycle as an analog of geoengineering. Geophys Res Lett 34:L15702

    Article  Google Scholar 

  13. Robock A, Liu Y (1994) The volcanic signal in Goddard Institute for Space Studies three-dimensional model simulations. J Clim l7:44–55

    Article  Google Scholar 

  14. Portman DA, Gutzler DS (1996) Explosive volcanic eruptions, the El Niño-Southern Oscillation, and U.S. climate variability. J Clim 9:17–33

    Article  Google Scholar 

  15. Xu Q (1986) The abnormal weather of China for summer 1980 and its relationship with the volcanic eruptions of Mount St. Helens. Acta Meteorol Sin 44:426–432 (in Chinese)

    Google Scholar 

  16. Shen CM, Wang W-C, Hao ZX et al (2007) Exceptional drought events over eastern China during the last five centuries. Clim Change 85:453–471

    Article  Google Scholar 

  17. Shen CM, Wang W-C, Hao ZX et al (2008) Characteristics of anomalous precipitation events over eastern China during the past five centuries. Clim Dyn 31:463–476

    Article  Google Scholar 

  18. Sato M, Hansen J, McCormic M et al (1993) Stratospheric aerosol optical depths, 1850–1990. J Geophys Res 98:2987–2994

    Google Scholar 

  19. Zhou TJ, Wu B, Wen XY et al (2008) A fast version of LASG/IAP climate system model and its 1000-year control integration. Adv Atmos Sci 25:655–672

    Article  Google Scholar 

  20. Wen XY, Zhou TJ, Wang SW et al (2007) Performance of a reconfigured atmospheric general circulation model at low resolution. Adv Atmos Sci 24:712–728

    Article  Google Scholar 

  21. Liu HL, Zhang XH, Li W et al (2004) An eddy-permitting oceanic general circulation model and its preliminary evaluations. Adv Atmos Sci 21:675–690

    Article  Google Scholar 

  22. Bonan GB, Oleson KW, Vertenstein M et al (2002) The land surface climatology of the Community Land Model coupled to the NCAR Community Climate Model. J Clim 15:3123–3149

    Article  Google Scholar 

  23. Briegleb BP, Bitz CM, Hunke EC et al (2004) Scientific description of the sea ice component in the Community Climate System Model: Version Three. NCAR Tech. 2004, Note NCARTN-463+STR

  24. Crowley T, Baum S, Kim K-Y et al (2003) Modeling ocean heat content changes during the last millennium. Geophys Res Lett 30:1932

    Article  Google Scholar 

  25. Ammann C, Joos F, Schimel D et al (2007) Solar influence on climate during the past millennium: results from transient simulations with the NCAR Climate System Model. Proc Natl Acad Sci USA 104:3713–3718

    Article  Google Scholar 

  26. Zhou TJ, Yu RC (2006) Twentieth century surface air temperature over China and the globe simulated by coupled climate models. J Clim 19:5843–5858

    Article  Google Scholar 

  27. Peng YB, Shen CM, Wang W-C et al (2010) Response of summer precipitation over eastern China to large volcanic eruptions. J Clim 23:818–824

    Article  Google Scholar 

  28. Li XD, Wang SW, Liu RX (1996) Advances in volcano-climatology. Seismol Geom Obs Res 17:74–80 (in Chinese)

    Google Scholar 

  29. Ammann C, Meehl G, Washington W et al (2003) A monthly and latitudinally varying volcanic forcing dataset in simulations of 20th century climate. Geophys Res Lett 30:1657

    Article  Google Scholar 

Download references

Acknowledgments

This work was supported by the National Natural Science Foundation of China (41305069), the Open Project Program of the Key Laboratory of Meteorological Disaster of Ministry of Education, Nanjing University of Information Science and Technology, China R&D Special Fund for Public Welfare Industry (meteorology) (GYHY201406020), and the National Basic Research Program of China (2010CB951904).

Conflict of Interest

The authors declare that they have no conflict of interest.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Tianjun Zhou.

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Man, W., Zhou, T. Response of the East Asian summer monsoon to large volcanic eruptions during the last millennium. Chin. Sci. Bull. 59, 4123–4129 (2014). https://doi.org/10.1007/s11434-014-0404-5

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11434-014-0404-5

Keywords

Navigation