Log in

Different roles of Ekman pum** in the west and east segments of the South China Sea Warm Current

  • Published:
Acta Oceanologica Sinica Aims and scope Submit manuscript

Abstract

A three-dimensional model is used to investigate the mechanism of the South China Sea (SCS) winter counter-current (also known as the SCS Warm Current, or the SCSWC), which flows against the wind. The model can reproduce the structure of the band-like currents over the northern shelf of the SCS, including the westward coastal current and slop current, and the SCSWC sandwiched in between. Sensitivity experiments are designed to understand the different roles of Ekman pum** of the SCSWC at different longitude. The results show that the Ekman pum** drives the SCSWC in the west segment. In the east, it is not the Ekman pum** but the intrusion of the Kuroshio that drives the SCSWC.

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 includes VAT (Germany)

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Blumberg A F, Mellor G L. 1987. A description of a three-dimensional coastal ocean circulation model. In: Heaps N S (Ed). Three-Dimensional Coastal Ocean Models, AGU Coastal and Estuarine Series, 4

  • Chiang T L, Wu C R, Chao S Y. 2008. Physical and geographical origins of the South China Sea Warm Current. Journal of Geophysical Research, 113, C08028, doi: 10.1029/2008JC004797

    Article  Google Scholar 

  • Carton J A, Giese B S. 2008. A reanalysis of ocean climate using SODA. Monthly Weather Review, 136: 2999–3017

    Article  Google Scholar 

  • Chao S Y, Shaw P T, Wang J. 1995. Wind relaxation as a possible cause of the South China Sea Warm Current. Journal of Oceanography, 51(1): 111–132

    Article  Google Scholar 

  • Fang G, Zhao B. 1989. A note on the main forcing of the northeastward flowing current off the southeast China coast. Progress in Oceanography, 21: 363–372

    Article  Google Scholar 

  • Flather R A. 1976. A tidal model of the northwest European continental shelf. Memoires Societe Royale des Sciences de Liege 6(10), 141–164

    Google Scholar 

  • Gan J P, Li H, Curchitser E N, et al. 2006. Modeling South China Sea circulation: Response to seasonal forcing regimes. Journal of Geophysical Research, 111, C06034, doi: 10.1029/2005JC003298

    Article  Google Scholar 

  • Guan B, Chen S. 1964. The current systems in the nearsea area of China Seas(in Chinese). Initial Report 5: 1–85

    Google Scholar 

  • Guan B. 1986. Evidence for a counter-wind current in winter off the southeast coast of China. Chinese Journal of Oceanology and Limnology 4(4), 319–332

    Article  Google Scholar 

  • Guan B. 1993. Winter counter-wind current off the southeastern China coast and a preliminary investigation of its source. Proceedings of the Symposium on the Physical and Chemical Oceanography of the China Seas. Bei**g: China Ocean Press, 1–9

    Google Scholar 

  • Guan B, Fang G. 2006. Winter Counter-wind Currents off the Southeastern China Coast: A Review. Journal of Oceanography, 62: 1–24

    Article  Google Scholar 

  • Guo Z, Yang T, Qiu D. 1985. The South China Sea Warm Current and the SW-ward current on its right side in winter. Tropical Oceanology(in Chinese), 4(1): 1–9

    Google Scholar 

  • Hong B, Wang D. 2006. Diagnostic analysis on the northern South China Sea winter counter-wind current. Chinese Science Bulletin, 51(supp II): 9–14

    Article  Google Scholar 

  • Hsueh Y, Zhong L. 2004. A pressure-driven South China Sea Warm Current. Journal of Geophysical Research, 109, C09014, doi: 10.1029/2004JC002374

    Article  Google Scholar 

  • Levitus S, Burgett R, Boyer T P. 1994a. World Ocean Atlas 1994 Volume 3: Salinity. NOAA Atlas NESDIS 3, U S Department of Commerce, Washington, D C, 99

    Google Scholar 

  • Levitus S, Boyer T P. 1994b. World Ocean Atlas 1994 Volume 4: Temperature. NOAA Atlas NESDIS 4, U S Department of Commerce, Washington D C, 117

    Google Scholar 

  • Liu, Yang Z H, Liu Q. 2000. Regional Dynamics of Seasonal Variability in the South China Sea. Journal of Physical Oceanography, 31: 272–284

    Article  Google Scholar 

  • Li Li, Wu Boyu. 1989. A Kuroshio loop in South China Sea?-on circulations of the northeastern South China Sea. Journal of oceanography in Taiwan Strait, 8(1): 89–95

    Google Scholar 

  • Marks K M, Smith W H F. 2006. An evaluation of publicity available global bathymetry grids. Marine Geophysical Researches, 27: 19–34

    Article  Google Scholar 

  • Ma H. 1987. On the winter circulation of the northern South China Sea and its relation to large oceanic current. Chinese Journal of Oceanology and Limnology, 5(1): 9–21

    Article  Google Scholar 

  • Pedlosky J. 1996. Ocean Circulation Theory. Spring-Verlag, 453

  • South China Sea Institute of Oceanology (SCSIO) (1985). Report on the Comprehensive Surveys and Studies in the South China Sea Region (II) (in Chinese). Bei**g: Science Press, 327

    Google Scholar 

  • Su J, Wang W. 1990. On the sources of the Taiwan Warm Current from the South China Sea. Donghai Marine Science, 8(3): 1–9

    Google Scholar 

  • Uppala S M, et al. 2005. The ERA-40 re-analysis. Quarterly Journal of the Royal Meteorological Society, 131: 2961–3012

    Article  Google Scholar 

  • Wang G, Chen D, Su J. 2006. Generation and life cycle of the dipole in the South China Sea summer circulation. Journal of Geophysical Research, 111, C06002, doi: 10.1029/2005JC003314

    Article  Google Scholar 

  • Wang D, Hong B, Gan J, et al. 2010. Numerical investigation on propulsion of the counter-wind current in the northern South China Sea in winter. Deep-Sea Research I, doi:10.1016/j.dsr.2102.06.07

  • Yang J, Wu D, Lin X. 2008. On the dynamics of the South China Sea Warm Current. Journal of Geophysical Research, 113, C08003, doi: 10.1029/2007JC004427

    Article  Google Scholar 

  • Zhong H L. 1990. Density-related current structures. In: Report of 10-year hydrographic section surveys of the northern China Sea continental shelf region and adjacent waters(in Chinese). Bei**g: China Ocean Press, 215–241

    Google Scholar 

  • Ye L F. 1994. On the mechanism of South China Sea Warm Current and Kuroshio Branch in winter C Preliminary results of 3-D baroclinic experiments. Terrestrial, Atmosphere and Ocean Sciences, 5(4): 597–610

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Dongxiao Wang.

Additional information

Foundation item: The Knowledge Innovation Program of the Chinese Academy of Sciences under contract No. KZCX1-YW-12-01; the National Science Fund for Distinguished Young Scholars under contract No. 40625017; the National Natural Science Foundation of China (Key Program) under contract No. 40830851; the National Program on Key Basic Research Project (973 Program) under contract No. 2007CB816004.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Wang, Q., Wang, Y., Bo, H. et al. Different roles of Ekman pum** in the west and east segments of the South China Sea Warm Current. Acta Oceanol. Sin. 30, 1–13 (2011). https://doi.org/10.1007/s13131-011-0113-8

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s13131-011-0113-8

Key words

Navigation