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Tidal distortion caused by the resonance of sexta‐diurnal tides in a micromesotidal embayment
Author(s) -
Song Dehai,
Yan Yuhan,
Wu Wen,
Diao Xiliang,
Ding Yang,
Bao Xianwen
Publication year - 2016
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
eISSN - 2169-9291
pISSN - 2169-9275
DOI - 10.1002/2016jc012039
Subject(s) - bay , oceanography , geology , harmonics , resonance (particle physics) , estuary , environmental science , physics , atomic physics , quantum mechanics , voltage
Double high water and double‐peak flood current were observed in Daya Bay (DYB), China, which is a shallow, mixed, mainly semidiurnal‐tide dominated bay with a micro to mesotidal range. Harmonic analysis reveals that the quarter and especially the sexta‐diurnal constituents are getting much stronger as tides propagating into the bay. The astronomical tides‐induced tidal asymmetry is yet dominant at the bay entrance but overtaken by the sexta‐diurnal tides at the end of the bay. Both the M 4 and M 6 tide meet the requirement proposed in previous studies but still unable to produce a double high water alone. Therefore, the conditions to produce a double high water between a fundamental tide and its higher harmonics need to be revisited. Analytical solutions were obtained in this paper, which fit the numerical solutions very well. Modeling result indicates M 6 alone with M 2 can produce the double high water in DYB but limited in some regions, while the combination of M 2 , M 4 , and M 6 tides would enhance the capability. The amplification of sexta‐diurnal tides in DYB is dominated by resonance and followed by shoaling effect. Bottom friction damped M 6 a lot and largely confined its amplification. However, the quadratic friction and other nonlinear processes are just responsible for about 10% of the total M 6 increase.