Articles | Volume 12, issue 2
Ocean Sci., 12, 517–531, 2016
Ocean Sci., 12, 517–531, 2016

Research article 08 Apr 2016

Research article | 08 Apr 2016

Tidal elevation, current, and energy flux in the area between the South China Sea and Java Sea

Zexun Wei et al.

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Short summary

Cited articles

Beardsley, R. C., Duda, T. F., Lynch, J. F., Irish, J. D., Ramp, S. R., Chiu, C. S., Tang, T. Y., Yang, Y. J., and Fang, G. H.: Barotropic tide in the northeast South China Sea, IEEE J. Ocean. Eng., 29, 1075–1086, 2004.
Cheng, Y. C. and Andersen, O. B.: Multimission empirical ocean tide modeling for shallow waters and polar seas, J. Geophys. Res., 116, C11001,, 2011.
Cressman, G. P.: An operational objective analysis system, Mon. Weather Rev., 87, 367–374, 1959.
Egbert, G. D. and Erofeeva, S. Y.: Efficient inverse modeling of barotropic ocean tides, J. Atmos. Ocean. Tech., 19, 183–204, 2002.
Fang, G. H.: Basic characteristics of the vertical structure of tidal currents – A comparison of theory and observations, Marine Sciences, 8, 1–11, 1984 (in Chinese with English abstract).

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Short summary
Harmonic constants of tides and tidal currents are obtained from long-term observations. Diurnal tides and tidal currents dominate in southern Natuna Sea and Karimata and Gaspar straits. Existing numerical model results are not accurate in the study area. Existing tidal models based on satellite observation need to be improved for the area.