Meteorology and Atmospheric Physics

, Volume 131, Issue 1, pp 105–113 | Cite as

Change in the relationship between the Australian summer monsoon circulation and boreal summer precipitation over Central China in the late 1990s

  • Ruowen Yang
  • Jian Wang
  • Tianyu Zhang
  • Shengping HeEmail author
Original Paper


Recent study revealed a close connection between the Australian summer monsoon (ASM) and boreal summer precipitation over Central China (SPCC). This study further revealed a strengthening of the ASM–SPCC relationship around the late 1990s. It is found that the relationship between the ASM and the SPCC during 1979–1997 (1998–2014) relationship is statistically insignificant (significant). Further analysis indicated that during 1998–2014, the weakened ASM is concurrent with significant positive sea surface temperature (SST) in the Indian Ocean and South China Sea, which could persist into the following boreal summer and further lead to intensified East Asian summer monsoon, strengthened western North Pacific subtropical high, and anomalous ascending motion over Central China. Consequently, more moisture is transported from the western Pacific northward to Central China where significant anomalous convergence appears. Therefore, the ASM could potentially influence the SPCC during 1998–2014. By contrast, the ASM-related SST and atmospheric circulation anomalies in boreal winter are statistically insignificant during 1979–1997. Such an interdecadal change might be attributed to the interdecadal warming that occurred in the Indian Ocean and South China Sea around the late 1990s. This study might be useful for the prediction of the SPCC.



This research was supported by the National Key Research and Development Program of China Grant No. 2017YFC1404000, the National Natural Science Foundation of China (41505073, 41405001, U1502233), the program of KLME1304, and the Jiangsu Collaborative Innovation Center for Climate Change.


  1. Chen M, Xie P, Janowiak JE et al (2002) Global land precipitation: a 50-yr monthly analysis based on gauge observations. J Hydrometeorol 3:249–266CrossRefGoogle Scholar
  2. Ding YH, Wang ZY, Sun Y (2008) Inter-decadal variation of the summer precipitation in East China and its association with decreasing Asian summer monsoon. Part I: observed evidences. Int J Climatol 28:1139–1161CrossRefGoogle Scholar
  3. Fan K (2006) Atmospheric circulation anomalies in the Southern Hemisphere and summer rainfall over Yangtze River Valley (in Chinese). Chin J Geophys 49:672–679Google Scholar
  4. Fan K, Wang HJ (2004) Antarctic oscillation and the dust weather frequency in North China. Geophys Res Lett 31:L10201. doi: 10.1029/2004GL019465 CrossRefGoogle Scholar
  5. Gong DY, Ho CH (2003) Arctic oscillation signals in the East Asian summer monsoon. J Geophys Res Atmos 108(D2):171–181CrossRefGoogle Scholar
  6. Gong DY, Yang J, Kim SJ, Gao Y, Guo D, Zhou T, Hu M (2011) Spring Arctic Oscillation-East Asian summer monsoon connection through circulation changes over the western North Pacific. Clim Dyn 37:2199–2216CrossRefGoogle Scholar
  7. He SP (2015) Potential connection between the Australian summer monsoon circulation and summer precipitation over central China. Atmos Ocean Sci Lett 8(3):120–126CrossRefGoogle Scholar
  8. He SP, Gao YQ, Li F, Wang HJ, He YC (2017) Impact of Arctic Oscillation on the East Asian climate: a review. Earth Sci Rev 164:48–62CrossRefGoogle Scholar
  9. He SP, Gao YQ, Furevik T, Wang HJ, Li F (2018) Teleconnection between sea ice in the Barents Sea in June and the Silk Road, Pacific-Japan and East Asian rainfall patterns in August. Adv Atmos Sci. doi: 10.1007/s00376-017-7029-y CrossRefGoogle Scholar
  10. Kalnay E, Kanamitsu M, Kistler R et al (1996) The NCEP/NCAR 40-year reanalysis project. Bull Am Meteorol Soc 77:437–471CrossRefGoogle Scholar
  11. Kwon MH, Jhun JG, Wang B, An SI, Kug JS (2005) Decadal change in relationship between east Asia and WPN summer monsoons. Geophys Res Lett 32:L16709. doi: 10.1029/2005GL02302 CrossRefGoogle Scholar
  12. Li HL, Wang HJ, Yin YZ (2012) Interdecadal variation of the West African summer monsoon during 1979–2010 and associated variability. Clim Dyn 39:2883–2894CrossRefGoogle Scholar
  13. Li F, Wang HJ, Gao YQ (2015) Modulation of Aleutian Low and Antarctic Oscillation co-variability by ENSO. Clim Dyn 44(5–6):1245–1256CrossRefGoogle Scholar
  14. Liebmann B, Smith CA (1996) Description of a complete (interpolated) outgoing longwave radiation dataset. Bull Am Meteorol Soc 77:1275–1277Google Scholar
  15. Liu G, Zhang Q, Sun S (2008) The relationship between circulation and SST anomaly East of Australia and the summer rainfall in the middle and lower reaches of the Yangtze River (in Chinese). Chin J Atmos Sci 32(2):231–241Google Scholar
  16. Smith TM, Reynolds RW, Peterson TC et al (2008) Improvements to NOAA’s historical merged land-ocean surface temperature analysis (1880–2006). J Clim 21:2283–2296CrossRefGoogle Scholar
  17. Sun JQ, Wang HJ, Yuan W (2008) A possible mechanism for the co-variability of the boreal spring Antarctic Oscillation and the Yangtze River valley summer rainfall. Int J Climatol 29:1276–1284CrossRefGoogle Scholar
  18. Wang H (2001) The weakening of the Asian monsoon circulation after the end of 1970’s. Adv Atmos Sci 18:376–386CrossRefGoogle Scholar
  19. Wang HJ, He SP (2015) The North China/Northeastern Asia severe summer drought in 2014. J Clim 28:6667–6681CrossRefGoogle Scholar
  20. Wang HJ, Matsuno T, Kurihara Y (2000) Ensemble Hindcast Experiments for the flood period over China in 1998 by use of the CCSR/NIES Atmospheric General Circulation Model. J Meteorol Soc Jpn 78:357–365CrossRefGoogle Scholar
  21. Wu Z, Wang B, Li J, Jin FF (2009) An empirical seasonal prediction model of the East Asian summer monsoon using ENSO and NAO. J Geophys Res Atmos 114(18):85–86Google Scholar
  22. Xie SP, Hu K, Hafner J, Tokinaga H, Du Y, Huang G, Sampe T (2009) Indian Ocean capacitor effect on Indo-western Pacific climate during the summer following El Niño. J Clim 22:730–747CrossRefGoogle Scholar
  23. Xue F, Wang HJ, He JH (2003a) Interannual variability of Mascarene high and Australian high and their influences on summer rainfall over East Asia. Chin Sci Bull 48(5):492–497CrossRefGoogle Scholar
  24. Xue F, Jiang DB, Lang XM, Wang HJ (2003b) Influence of the Mascarene high and Australian high on the summer monsoon in East Asia: ensemble simulation. Adv Atmos Sci 20(5):799–809CrossRefGoogle Scholar
  25. Xue F, Wang HJ, He JH (2004) Interannual variability of Mascarene high and Australian high and their influences on East Asian summer monsoon. J Meteorol Soc Jpn 82(4):1173–1186CrossRefGoogle Scholar
  26. Zhang C, Zhang H (2010) Potential impacts of East Asian winter monsoon on climate variability and predictability in the Australian summer monsoon region. Theor Appl Climatol 101(1):161–177CrossRefGoogle Scholar
  27. Zhang R, Sumi A, Kimoto M (1996) Impact of El Niño on the East Asian monsoon: a diagnostic study of the ‘86/87 and ‘91/92 events. J Meteorol Soc Jpn 74:49–62CrossRefGoogle Scholar
  28. Zhu YL, Wang HJ (2010) The relationship between the Aleutian Low and the Australian summer monsoon at interannual time scales. Adv Atmos Sci 27(1):177–184CrossRefGoogle Scholar

Copyright information

© Springer-Verlag GmbH Austria 2017

Authors and Affiliations

  • Ruowen Yang
    • 1
    • 2
  • Jian Wang
    • 1
  • Tianyu Zhang
    • 3
  • Shengping He
    • 4
    Email author
  1. 1.Department of Atmospheric ScienceYunnan UniversityKunmingPeople’s Republic of China
  2. 2.Key Laboratory of Meteorological Disaster of Ministry of EducationNanjing University of Information Science and TechnologyNanjingPeople’s Republic of China
  3. 3.Chongqing Climate CenterChongqingPeople’s Republic of China
  4. 4.Geophysical Institute, Bjerknes Centre for Climate ResearchUniversity of BergenBergenNorway

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