The divergence-convergence effect of surface current and its action on the Bohai Sea

Zhao Jinping; Shi Maochong

doi:10.1007/BF02850820

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The divergence-convergence effect of surface current and its action on the Bohai Sea

Updated：2023-05-16

- The divergence-convergence effect of surface current and its action on the Bohai Sea
- Journal of Oceanology and Limnology Vol. 11, Issue 2, Pages: 135-142(1993)
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
- DOI：10.1007/BF02850820
  CLC：
- Published：1993
- Accepted：
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Jinping, Z., Maochong, S. The divergence-convergence effect of surface current and its action on the Bohai Sea., Chin. J. Ocean. Limnol. 11, 135–142 (1993). https://doi.org/10.1007/BF02850820
DOI：

Jinping, Z., Maochong, S. The divergence-convergence effect of surface current and its action on the Bohai Sea., Chin. J. Ocean. Limnol. 11, 135–142 (1993). https://doi.org/10.1007/BF02850820 DOI：

摘要

Abstract

The action of the wind field and the influence of topography can cause divergence or convergence of surface current. The existence of the divergence-convergence effect is proved and the dynamical significance of the divergent or convergent state and its link with many marine phenomena are pointed out. Divergence fields of surface current in the Bohai Sea in winter and summer are obtained by numerical modelling describing the divergence-convergence character of seasonally wind-driven current. The relation between the effect and seasonal marine phenomena is discussed. Study on the divergence-convergence effect of surface current (DCESC) can be an indirect method for testing the calculated results.

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references

Guan Bingxian. 1962. On some problems of currents in Chinese Seas.Oceanol. et Limnol. Sinica 4 (3): 121–141 (in Chinese with English abstract)

Zhang Fangjian. 1986. Chinese Ice in the Sea. Ocean Press, Beijing, 165pp. (in Chinese)

Zhao Jinping & Shi Maochong, 1993. Numerical modelling of three-dimension characteristics of wind-driven current in the Bohai Sea.Chin. J. Oceanol. Limnol. 11(1).

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