With the fine horizontal (5' x 5') and vertical (15 levels) grids, a three-
dimensional model, imbedded a closure turbulence sub-model, was used to cal
culate the barotropic tides and tidal currents in the Bohai Sea, Yellow Sea
, and East China Sea. The computational results are in good agreement with
the observed M2, S2, K1 and O1 tides in the domain. Comparison with fifty t
ide gauges showed that the averaged absolute differences between the simula
ted and observed amplitudes are only 3.95, 2.96, 2.5 and 1.78 cm for the M2
, S2, K1 and O1 tidal waves, respectively. The averaged phase-lag differenc
es of the four tides are 6.88, 6.96, 5.96 and 6.16 degrees. The model repro
duces well the tidal charts and this characteristic is discussed in detail.
Comparison with 13 current stations, gave averaged absolute deviations bet
ween the calculated and observed harmonic constant of the eastern and north
ern tidal current of [6.53, 20.4, 7.55, 24.9]; [3.24, 24.2, 2.89, 22.8]; [2
.98, 22.4, 3.6, 25.9]; [2.39, 35.8, 2.01 cm s(-1), 22.6 degrees] for M2, S2
, K1 and O1, respectively. The calculated structures of the tidal current e
llipse in the vertical are in fair agreement with the observations. The sur
face distributions of the tidal current ellipse in the four tidal systems a
nd the maximum current distributions are discussed in detail. (C) 2001 Ifre
mer/CNRS/IRD/Editions scientifiques et medicales Elsevier SAS.