Chinese Science Bulletin

, Volume 55, Issue 26, pp 3001–3007 | Cite as

1876–1878 severe drought in North China: Facts, impacts and climatic background

  • ZhiXin Hao
  • JingYun Zheng
  • GuoFeng Wu
  • XueZhen Zhang
  • QuanSheng GeEmail author
Article Geography


Based on the reconstructed precipitation series in North China from historical documents, the 1876–1878 drought was identified as the most severe and extreme one in North China over the past 300 years. Meanwhile, the spatial patterns of seasonal and annual precipitation during 1876–1877 were analyzed and the social and economic impacts related with this drought event were evaluated according to the descriptions in the historical documents. The results indicated that this long-lasting drought started by the spring of 1876 and did not stop until the spring of 1878. Within the three years, the harvest failures brought the rice price increased to 5–10 times than that in the normal year, and the total population in the five provinces over North China decreased by more than 20 million due to a large number of dead people and migrations. In addition, related investigations suggested that the 1876–1878 drought was prevalent worldwide, which has possible link with abnormal high SST in the equatorial central and eastern Pacific, strong El Niño episode and positive AAO anomalies.


1876–1878 severe drought North China social impact climatic background 


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  1. 1.
    Fye F K, Stahle D W, Cook E R. Paleoclimatic analogs to twentieth-century moisture regimes across the United States. Bull Amer Meteorol Soc, 2003, 84:901–909CrossRefGoogle Scholar
  2. 2.
    Woodhouse C A, Overpeck J T. Two thousand years of drought variability in central United States. Bull Amer Meteorol Soc, 1998, 79:2693–2714CrossRefGoogle Scholar
  3. 3.
    Ma Z J, Gao Q H. Climate changes of China in the quaternary period and analysis on drought disasters of North China in the future (in Chinese). Quat Sci, 2004, 24:245–251Google Scholar
  4. 4.
    Aceituno P, Prieto M D, Solari M E, et al. The 1877–1878 El Niño episode: Associated impacts in South America. Clim Change, 2009, 92:389–416CrossRefGoogle Scholar
  5. 5.
    Zheng J Y, Wang W C, Ge Q S, et al. Precipitation variability and extreme events in eastern China during the past 1500 years. Terr Atmos Ocean Sci, 2006, 17:579–592Google Scholar
  6. 6.
    Man Z M. Climatic background of the severe drought in 1877 (in Chinese). Fudan J (Social Sci), 2000, 6:28–35Google Scholar
  7. 7.
    Zhang D. Variation of dry-wet climate and severe drought events as revealed in the climate records of China over the past 1000 years (in Chinese). Sci Technol Rev, 2004, 8:47–49Google Scholar
  8. 8.
    Liang E Y, Shao X M, Kong Z C, et al. The extreme drought in the 1920s and its effect on tree growth deduced from tree ring analysis: A case study in North China. Ann For Sci, 2003, 60:145–152CrossRefGoogle Scholar
  9. 9.
    Zheng J Y, Hao Z X, Ge Q S. Reconstruction of annual precipitation in the middle and lower reaches of the Yellow River for the last 300 years. Sci China Ser D-Earth Sci, 2005, 48:2182–2197CrossRefGoogle Scholar
  10. 10.
    Chinese Academy of Meteorological Sciences. Yearly Charts of Dryness/Wetness in China for the Last 500-Year Period (in Chinese). Beijing: Map Press, 1981. 209–210Google Scholar
  11. 11.
    Dai A, Trenberth K E, Qian T. A global data set of Palmer Drought Severity Index for 1870–2002: Relationship with soil moisture and effects of surface warming. J Hydrometeorol, 2004, 5:1117–1130CrossRefGoogle Scholar
  12. 12.
    Zhang P Y. Historical climate change in China (in Chinese). Jinan: Shandong Science and Technology Press, 1996. 533Google Scholar
  13. 13.
    Smith T M, Reynolds R W. Extended reconstruction of global sea surface temperatures based on COADS data (1854–1997). J Clim, 2003, 16:1495–1510CrossRefGoogle Scholar
  14. 14.
    Zhang D. A Compendium of Chinese Meteorological Records of the Last 3000 Years (in Chinese). Nanjing: Jiangsu Education Press, 2004. 3343–3407Google Scholar
  15. 15.
    Cao S J. History of Population in China (Vol. 5, Qing Dynasty) (in Chinese). Shanghai: Fudan University Press, 2001. 647–689Google Scholar
  16. 16.
    He H W. The Great North China Drought Famine in the Early Guangxu Reign (1876–1879) (in Chinese). Hongkong: The Chinese University Press, 1980. 33Google Scholar
  17. 17.
    Gao L C. The historical reason of the northeast immigration in modern China (in Chinese). J Northeast Normal Univ (Social Sci), 2005, 2:29–35Google Scholar
  18. 18.
    Nicholls N. Historical El Niño/Southern Oscillation variability in the Australasian region. In: Diaz H F, Markgraf V, eds. El Niño Historical and Paleoclimatic Aspects of the Southern Oscillation. Cambridge: Cambridge University Press, 1992. 151–174Google Scholar
  19. 19.
    Herweijer C, Seager R, Cook E R. North American droughts of the mid to late nineteenth century: A history, simulation and implication for mediaeval drought. Holocene, 2006, 16:159–171CrossRefGoogle Scholar
  20. 20.
    Kiladis G N, Diaz H F. An analysis of the 1877–78 ENSO episode and comparison with 1982–83. Mon Weather Rev, 1986, 114: 1035–1047CrossRefGoogle Scholar
  21. 21.
    Quinn W H. A study of Southern Oscillation-related climatic activity for AD 622-1900 incorporating Nile River flood data. In: Diaz H F, Markgraf V, eds. El Niño Historical and Paleoclimatic Aspects of the Southern Oscillation. Cambridge: Cambridge University Press, 1992. 119–149Google Scholar
  22. 22.
    Gergis J L, Fowler A M. A history of ENSO events since AD 1525: Implications for future climate change. Clim Change, 2009, 92: 343–387CrossRefGoogle Scholar
  23. 23.
    D’Arrigo R, Allan R, Wilson R, et al. Pacific and Indian Ocean climate signals in a tree-ring record of Java monsoon drought. Int J Climatol, 2008, 28:1889–1901CrossRefGoogle Scholar
  24. 24.
    Lu R Y. Interannual variation of North China rainfall in rainy season and SSTs in the equatorial eastern Pacific. Chinese Sci Bull, 2005, 50:2069–2073CrossRefGoogle Scholar
  25. 25.
    Li X P, Luo Y, Guo P W, et al. Relationship of the SSTA temporal variation in the middle and east equatorial Pacific in spring and summer to East Asia summer monsoon (in Chinese). J Appl Meteorol Sci, 2006, 17:176–182Google Scholar
  26. 26.
    Wang H J, Fan K. Central-north China precipitation as reconstructed from the Qing dynasty: Signal of the Antarctic Atmospheric Oscillation. Geophys Res Lett, 2005, 32,L24705, doi:10.1029/2005GL024562Google Scholar
  27. 27.
    Fan K, Wang H J. The anomalous Antarctic Oscillation and the summer precipitation over Eastern China in 2006 (in Chinese). J Appl Meteorol Sci, 2006, 17:383–384Google Scholar
  28. 28.
    Ma Z G. The interdecadal dry/wet trend and shift of North China and their relationship to the Pacific Decadal Oscillation (PDO). Chinese Sci Bull, 2007, 50:2130–2139CrossRefGoogle Scholar

Copyright information

© Science China Press and Springer-Verlag Berlin Heidelberg 2010

Authors and Affiliations

  • ZhiXin Hao
    • 1
  • JingYun Zheng
    • 1
  • GuoFeng Wu
    • 1
    • 2
  • XueZhen Zhang
    • 1
  • QuanSheng Ge
    • 1
    Email author
  1. 1.Institute of Geographic Sciences and Natural Resources ResearchChinese Academy of SciencesBeijingChina
  2. 2.Graduate University of Chinese Academy of SciencesBeijingChina

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