Skip to main content
Log in

Does the Asian monsoon modulate tropical cyclone activity over the South China Sea?

  • Published:
Chinese Journal of Oceanology and Limnology Aims and scope Submit manuscript

Abstract

To investigate whether the Asian monsoon influences tropical cyclone (TC) activity over the South China Sea (SCS), TCs (including tropical storms and typhoons) over the SCS are analyzed using the Joint Typhoon Warning Center dataset from 1945 to 2009. Results show an increasing trend in the frequencies of TC-all (all TCs over the SCS) and TY-all (all typhoons over the SCS), due mainly to an increase in the number of TCs moving into the SCS after development elsewhere. Little change is seen in the number of TCs that form in the SCS. The results of wavelet analysis indicate that the frequency of typhoons (TY) shows a similar oscillation as that of TCs, i.e., a dominant periodicity of 8–16 years around the 1970s for all TC activity, except for TC-mov (TCs that moved into the SCS from the western North Pacific). To examine the relationship between typhoon activity and the summer monsoon, a correlation analysis was performed that considered typhoons, TCs, and five monsoon indexes. The analysis reveals statistically significant negative correlation between the strength of the Southwest Asian summer monsoon and typhoon activity over the SCS, which likely reflects the effect of the monsoon on TC formation in the western North Pacific (WNP) and subsequent movement into the SCS. There is a statistically significant negative correlation between TY-loc (typhoons that developed from TCs formed over the SCS) and the South China Sea summer monsoon and Southeast Asian summer monsoon.

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

  • Chan J C L. 2000. Tropical cyclone activity over the western North Pacific associated with El Niño and La Niña events. J. Clim., 13: 2 960–2 972.

    Google Scholar 

  • Chen T, Weng S-P, Yamazaki N, Kiehne S. 1998. Interannual variation in the tropical cyclone formation over the western North Pacific. Mon. Wea. Rev., 126: 1 080–1 090.

    Google Scholar 

  • Chen G, Huang R. 2008. Influence of monsoon over the warm pool on interannual variation on tropical cyclone activity over the western North Pacific. Adv. Atmos. Sci., 25 (2): 319–328.

    Article  Google Scholar 

  • Chen G. 2011. How does shifting Pacific Ocean warming modulate on tropical cyclone frequency over the South China Sea? J. Clim., 24: 4 695–4 700.

    Google Scholar 

  • Ho C H, Baik J J, Kim J H, Gong D Y, Sui C H. 2004. Interdecadal changes in summertime typhoon tracks. J. Clim., 17: 1 767–1 776.

    Article  Google Scholar 

  • Gray W M. 1975. Tropical cyclone genesis. Dept. of Atmos. Sci. Paper No. 232, Colorado State University, Ft. Collins, Co. 121p.

    Google Scholar 

  • Gray W M. 1998. The formation of tropical cyclones. Meteor. Atmos. Phys., 67: 37–69.

    Article  Google Scholar 

  • Lee C-S, Lin Y-L, Cheung K K W. 2006. Tropical cyclone formations in the South China Sea associated with the Mei-Yu Front. Mon. Wea. Rev., 134: 2 670–2 687.

    Google Scholar 

  • Li J P, Zeng Q C. 2000. Significance of the normalized seasonality of wind field and its rationality for characterizing the monsoon. Sci. Chin. D, 43: 646–653.

    Article  Google Scholar 

  • Li J, Zeng Q. 2002. A unified monsoon index. Geophys. Res. Lett., 29 (8): 1 151–1 154.

    Article  Google Scholar 

  • Li J P, Zeng Q C. 2003. A new monsoon index and the geographical distribution of the global monsoons. Adv. Atmos. Sci., 20: 299–302.

    Article  Google Scholar 

  • Kuma V, Krishnan R. 2005. On the association between the Indian summer monsoon and the tropical cyclone activity over northwest Pacific. Curr. Sci., 88: 602–612.

    Google Scholar 

  • Sreenivas P, Gnanaseelan C, Prasad K V S R. 2012. Influence of El Niño and Indian Ocean Dipole on sea level variability in the Bay of Bengal. Global and Planetary Change, 80–81: 215–225.

    Article  Google Scholar 

  • Torrence C, Compo G P. 1998. A practical guide to wavelet analysis. B. Am. Meteorol. Soc., 70: 61–78.

    Article  Google Scholar 

  • Wang H, Ding Y H, He J H. 2006. Influence of western North Pacific summer monsoon changes on typhoon geneis. Acta Meteorologica Sinica, 64: 345–356. (in Chinese)

    Google Scholar 

  • Wang B, Fan Z. 1999. Choice of South Asian summer monsoon indices. Bull. Amer. Meteor. Soc., 80: 629–638.

    Article  Google Scholar 

  • Wang G, Wang H, Qi Y. 2007a. Seasonal variability of tropical cyclones generated over the South China Sea. Acta Oceanologica Sinica, 26(4): 20–28.

    Google Scholar 

  • Wang G, Su J, Ding Y, Chen D. 2007b. Tropical cyclones genesis over the South China Sea. J. Mar. Syst., 68(3–4): 318–326.

    Article  Google Scholar 

  • Wang L, Fung C-H, Lau K-H. 2007c. The upper ocean thermal structure and the genesis locations of tropical cyclones in the South China Sea. Journal of Ocean University of China, 6 (2): 125–131.

    Article  Google Scholar 

  • Wang L, Lau K-H, Fung C-H, Gan J P. 2007d. The relative vorticity of ocean surface winds from the QuikSCAT satellite and its effects on the geneses of tropical cyclones in the South China Sea. Tellus, A, 59: 562–569.

    Article  Google Scholar 

  • Wang L, Lau K-H, Zhang Q-H, Fung C-H. 2008. Observation of non-developing and developing tropical disturbances over the South China Sea using SSM/I satellite. Geophys. Res. Lett., 35: L10802.

    Article  Google Scholar 

  • Wu L, Wang B, Geng S. 2005. Growing typhoon influence on East Asia. Geophys. Res. Lett., 32: L18703.

    Article  Google Scholar 

  • Zeng Q C, Zhang B L. 1998. On the seasonal variation of atmospheric general circulation and the monsoon. Chin. J. Atmo s. Sci., 23 (3): 211–220.

    Google Scholar 

  • Zhou T, Wu B, Scaife A A, Bronnimann S et al. 2009a. The CLIVAR C20C Project: which components of the Asian-Australian monsoon circulation variations are forced and reproducible? Climate Dynamics, 33 (7–8): 1 051–1 068.

    Google Scholar 

  • Zhou T, Yu R, Zhang J et al. 2009b. Why the western Pacific subtropical high has extended westward since the late 1970s. J. Climate, 22: 2 199–2 215.

    Google Scholar 

  • Zhou T, Gong D, Li J, Li B. 2009c. Detecting and understanding the multi-decadal variability of the East Asian Summer Monsoon—recent progress and state of affairs. Meteorologische Zeitschrift, 18(4): 455–467.

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Yuping Guan  (管玉平).

Additional information

Supported by the Knowledge Innovation Program of Chinese Academy of Sciences (No. KZCX2-YW-Q11-02)

Rights and permissions

Reprints and permissions

About this article

Cite this article

Huang, Q., Guan, Y. Does the Asian monsoon modulate tropical cyclone activity over the South China Sea?. Chin. J. Ocean. Limnol. 30, 960–965 (2012). https://doi.org/10.1007/s00343-012-1273-x

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00343-012-1273-x

Keyword

Navigation