A wave-tide-circulation coupled model based on Princeton Ocean Model is
established to study the seasonal circulation in the Malay Peninsula Eastern
Continental Shelf region. The model successfully reconstructs the observed
seasonal variation of the circulation in the region, as well as the main currents.
The simulated tidal harmonic constants, sea surface temperature, and sea
surface height anomaly agree with the observations well.

Categories: Air, Hidrodinamik (Pasang Surut), Marin
Tags: Artikel Jurnal, Data Penerbitan, Sulit