Log in

The Effect of Boreal Summer Intraseasonal Oscillation on Mixed Layer and Upper Ocean Temperature over the South China Sea

  • Published:
Journal of Ocean University of China Aims and scope Submit manuscript

Abstract

Intraseasonal oscillation of the mixed layer and upper ocean temperature has been found to occur over the South China Sea (SCS) in the summer monsoon season based on the multiple reanalysis and observational data in this study. The method of composite analysis and an upper ocean temperature equation assisted the analysis of physical mechanisms. The results show that the mixed layer depth (MLD) in the SCS has a significant oscillation with a 30–60 d period over the SCS region, which is closely related to boreal summer intraseasonal oscillation (BSISO) activities. The MLD can increase (decrease) during the positive (negative) phase of the BSISO and usually lags behind by approximately one-eighth of the lifecycle (5 days) of the BSISO-related convection. The BSISO may cause periodic anomalies at the air-sea boundary, such as wind stress and heat flux, so it can play a dominant role in modulating the variation in MLD. There also are significant intraseasonal seawater temperature anomalies in both the surface and subsurface layers of the SCS. In addition, during the initial phase of the BSISO, the temperature anomaly signals of the thermocline are obviously opposite to the sea surface temperature (SST), especially in the southern SCS. According to the results from the analysis of the temperature equation, the vertical entrainment term caused by BSISO-related wind stress is stronger than the thermal forcing during the initial stage of convection, and it is more significant in the southern SCS.

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

Access this article

Subscribe and save

Springer+ Basic
EUR 32.99 /Month
  • Get 10 units per month
  • Download Article/Chapter or Ebook
  • 1 Unit = 1 Article or 1 Chapter
  • Cancel anytime
Subscribe now

Buy Now

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

  • An, Y. Z., Zhang, R., Wang, H. Z., Chen-Jian, and Chen, Y. D., 2012. Study on calculation and spatio-temporal variations of global ocean mixed layer depth. Chinese Journal of Geophysics, 55(7): 2249–2258 (in Chinese with English abstract).

    Google Scholar 

  • Anderson, S. P., Weller, R. A., and Lukas, R. B., 1996. Surface buoyancy forcing and the mixed layer of the western Pacific warm pool: observations and 1d model results. Journal of Climate, 9(12): 3056–3085.

    Article  Google Scholar 

  • Annamalai, H., and Slingo, J. M., 2001. Active/break cycles: Diagnosis of the intraseasonal variability of the Asian summer monsoon. Climate Dynamics, 18(1–2): 85–102.

    Article  Google Scholar 

  • Chassignet, E. P., Hulburt, H. E., Smedstad, O. M., Halliwell, G. R., and Hogan, P. J., 2007. The HYCOM (hybrid coordinate ocean model) data assimilative system. Journal of Marine Systems, 65(1–4): 60–83.

    Article  Google Scholar 

  • Chen, X., Li, C., and Li, X., 2020. Influences of ENSO on boreal summer intraseasonal oscillation over the western Pacific in decaying summer. Climate Dynamics, 54(7–8): 3461–3473.

    Article  Google Scholar 

  • Duvel, J. P., and Vialard, J., 2007. Indo-Pacific sea surface temperature perturbations associated with intraseasonal oscillations of tropical convection. Journal of Climate, 20(13): 3056–3082.

    Article  Google Scholar 

  • Girishkumar, M. S., Ravichandran, M., and Mcphaden, M. J., 2013. Temperature inversions and their influence on the mixed layer heat budget during the winters of 2006–2007 and 2007–2008 in the Bay of Bengal. Journal of Geophysical Research: Oceans, 118(5): 2426–2437.

    Article  Google Scholar 

  • Hsu, H. H., and Weng, C. H., 2000. Northwestward propagation of the intraseasonal oscillation in the western North Pacific during the boreal summer: Structure and mechanism. Journal of Climate, 14(18): 3834–3850.

    Article  Google Scholar 

  • Huang, B. Y., Xue, Y., Zhang, D. X., Kumar, A., and McPhaden, M. J., 2010. The NCEP GODAS ocean analysis of the Tropical Pacific mixed layer heat budget on seasonal to inter-annual time scales. Journal of Climate, 23(18): 4901–4925.

    Article  Google Scholar 

  • Jia, W. T., Zhang, W. M., Zhu, J. H., and Sun, J. L., 2020. The effect of boreal summer intraseasonal oscillation on evaporation duct and electromagnetic propagation over the South China Sea. Atmosphere, 11(12): 1298.

    Article  Google Scholar 

  • Jiang, X., Li, T., and Wang, B., 2004. Structures and mechanisms of the northward propagating boreal summer intraseasonal oscillation. Journal of Climate, 17(5): 1022–1039.

    Article  Google Scholar 

  • Kessler, W. S., and Kleeman, R., 2000. Rectification of the Madden-Julian oscillation into the ENSO cycle. Journal of Climate, 43(13): 3560–3575.

    Article  Google Scholar 

  • Lawrence, D. M., and Webster, P. J., 2002. The boreal summer intraseasonal oscillation: Relationship between northward and eastward movement of convection. Journal of the Atmospheric Sciences, 59(9): 1593–1606.

    Article  Google Scholar 

  • Lee, J. Y., Wang, B., Wheeler, M. C., Fu, X., Waliser, D. E., and Kang, I. S., 2013. Real-time multivariate indices for the boreal summer intraseasonal oscillation over the Asian summer monsoon region. Climate Dynamics, 40(1–2): 493–509.

    Article  Google Scholar 

  • Lukas, R., and Lindstrom, E., 1991. The mixed layer of the western equatorial Pacific Ocean. Journal of Geophysical Research, 96(S01): 3343.

    Article  Google Scholar 

  • Matthews, A. J., Singhruck, P., and Heywood, K. J., 2007. Deep ocean impact of a Madden-Julian Oscillation observed by Argo floats. Science, 318(5857): 1765–1769.

    Article  Google Scholar 

  • Matthews, A. J., Singhruck, P., and Heywood, K. J., 2010. Ocean temperature and salinity components of the Madden-Julian oscillation observed by Argo floats. Climate Dynamics, 35(7–8): 1149–1168.

    Article  Google Scholar 

  • Paulson, E. A., 1977. Irradiance measurements in the upper ocean. Journal of Physical Oceanography, 7(6): 952–956.

    Article  Google Scholar 

  • Qiu, B., 2002. The Kuroshio extension system: Its large-scale variability and role in the midlatitude ocean-atmosphere interaction. Journal of Oceanography, 58(1): 57–75.

    Article  Google Scholar 

  • Reynolds, R. W., Smith, T. M., Liu, C., Chelton, D. B., Casey, K. S., and Schlax, M. G., 2007. Daily high-resolution-blended analyses for sea surface temperature. Journal of Climate, 20(22): 5473–5496.

    Article  Google Scholar 

  • Roxy, M., and Tanimoto, Y., 2012. Influence of sea surface temperature on the intraseasonal variability of the South China Sea summer monsoon. Climate Dynamics, 39(5): 1209–1218.

    Article  Google Scholar 

  • Roxy, M., Tanimoto, Y., Preethi, B., Terray, P., and Krishnan, R., 2013. Intraseasonal SST-precipitation relationship and its spatial variability over the tropical summer monsoon region. Climate Dynamics, 41(1): 45–61.

    Article  Google Scholar 

  • Stevenson, J. W., and Niiler, P. P., 1983. Upper ocean heat budget during the Hawaii-to-Tahiti shuttle experiment. Journal of Physical Oceanography, 13(10): 1894–1907.

    Article  Google Scholar 

  • Sun, C. X., Liu, Q. Y., and Jia, Y. L., 2007. Annual and inter-annual variations of the mixed layer in the South China Sea. Periodical of Ocean University of China, 37(2): 197–203 (in Chinese with English abstract).

    Google Scholar 

  • Wang, B., and **e, X., 1997. A model for the boreal summer intraseasonal oscillation. Journal of the Atmospheric Sciences, 54(1): 72–86.

    Article  Google Scholar 

  • Wang, T., Yang, X. Q., Fang, J., Sun, X., and Ren, X., 2018. Role of air-sea interaction in the 30–60-day boreal summer intraseasonal oscillation over the western North Pacific. Journal of Climate, 31(4): 1653–1680.

    Article  Google Scholar 

  • Webber, B. G., Matthews, A. J., and Heywood, K. J., 2010. A dynamical ocean feedback mechanism for the Madden-Julian oscillation. Quarterly Journal of the Royal Meteorological Society: A Journal of the Atmospheric Sciences, Applied Meteorology and Physical Oceanography, 136(648): 740–754.

    Google Scholar 

  • Wu, W., Tomczak, M., Fang, X., and Wu, D., 2001. The barrier layer in the southern region of the South China Sea. Chinese Science Bulletin, 46(16): 1388–1392.

    Article  Google Scholar 

  • Ye, K., and Wu, R., 2015. Contrast of local air-sea relationships between 10–20-day and 30–60-day intraseasonal oscillations during May–September over the South China Sea and western North Pacific. Climate Dynamics, 45(11): 3441–3459.

    Article  Google Scholar 

  • Yu, L., **, X., and Weller, R. A., 2008. 2008: Multidecade global flux datasets from the Objectively Analyzed Air-Sea Fluxes (OAFlux) Project: Latent and sensible heat fluxes, ocean evaporation, and related surface meteorological variables. OAFlux Project Tecnology Report. Woods Hole Oceanographic Institution, OA-2008-1.

  • Zu, T., Xue, H., Wang, D., Geng, B., Zeng, L., Liu, Q., et al., 2019. Interannual variation of the South China Sea circulation during winter: Intensified in the southern basin. Climate Dynamics, 52(3): 1917–1933.

    Article  Google Scholar 

Download references

Acknowledgement

This study was supported by the National Natural Science Foundation of China (No. 41830964).

Author information

Authors and Affiliations

Authors

Corresponding authors

Correspondence to Jilin Sun or Weimin Zhang.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Jia, W., Sun, J., Zhang, W. et al. The Effect of Boreal Summer Intraseasonal Oscillation on Mixed Layer and Upper Ocean Temperature over the South China Sea. J. Ocean Univ. China 22, 285–296 (2023). https://doi.org/10.1007/s11802-023-5008-8

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11802-023-5008-8

Key words

Navigation