The four leading tidal constituents M2, S2, K1 and O1 in the South China Sea are simulated by using POM. The model is forced with tide-generating potential and
On the basis of data of drifting bottles'tracks and the current measured in anchored stations, as well as temperature and salinity observed in cruise invest
By using wide scope ADCP data which were got during SCSMEX (South China Sea Monsoon Experiment) period in the summer of 1998, and comparing these data with nume