Ocean Science
Ocean Science
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Articles | Volume 16, issue 1
Articles | Volume 16, issue 1
https://doi.org/10.5194/os-16-1-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-16-1-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 16, issue 1
Research article
 | 
06 Jan 2020
Research article |  | 06 Jan 2020

Seasonal variation of the principal tidal constituents in the Bohai Sea

Daosheng Wang, Haidong Pan, Guangzhen Jin, and Xianqing Lv

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Cited articles

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Arbic, B. K., Karsten, R. H., and Garrett, C.: On tidal resonance in the global ocean and the back-effect of coastal tides upon open-ocean tides, Atmos. Ocean, 47, 239–266, 2009. 
Chavez, F. P., Strutton, P. G., Friederich, G. E., Feely, R. A., Feldman, G. C., Foley, D. G., and Mcphaden, M. J.: Biological and Chemical Response of the Equatorial Pacific Ocean to the 1997–98 El Niño, Science, 286, 2126–2131, 1999. 
Codiga, D. L.: Unified tidal analysis and prediction using the UTide Matlab functions, Graduate School of Oceanography, University of Rhode Island, Narragansett, RI, 2011. 
Colosi, J. A. and Munk, W.: Tales of the venerable Honolulu tide gauge, J. Phys. Oceanogr., 36, 967–996, 2006. 
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This work investigates the seasonal variations of M2, S2, K1, and O1 at E2 and Dalian. At E2, the M2 amplitude and phase lag reach maximum in summer and minimum in winter. The S2 and K1 amplitudes show annual cycles, while the phase lags of S2, K1, and O1 had semi-annual cycles. The seasonal variations at Dalian are different from those at E2, except for M2 phase lag. The seasonal variations at E2 are induced by seasonality of vertical eddy viscosity, while those at Dalian cannot be explained.
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