Between 1989 and 1991 the authors made observations that confirm and elucid
ate the coupling between harbor seiches at Puerto Princesa on Palawan Islan
d in the Philippines and tide-generated internal solitons in the Sulu Sea.
Published tidal current predictions for Basilan Strait in the Sulu Archipel
igo were used to produce an index to the daily ebb tidal flows near Pearl B
ank where the solitons originate. The coherence between predicted maximum e
bb tidal current speed and observed seiche activity was 0.60 and the phase
lag between the two quantities closely marched published estimates of the t
ime required for solitons to cross the Sulu Sea. Arrival of the Sulu Sea wa
ves immediately offshore of Puerto Princesa in the form of internal bores c
orresponded in time to the initiation of harbor seiche activity. A more pre
cise estimate of soliton travel time was determined from the time differenc
e between predicted maximum ebb current and the initiation of seiche activi
ty, and it was found to have a remarkably regular seasonal pattern, which c
an be largely explained by seasonal variations in Sulu Sea temperature and
salinity stratification. Therefore, the timing of seiche events at Puerto P
rincesa can be forecast based on Sulu Archipeligo ride predictions and soli
ton travel time. In general, the fortnightly pattern of seiche magnitude fo
llows that of tidal current predictions, but day-to-day deviations are comm
on. Seiche magnitude varies seasonally with generally low activity during t
he winter (northeast) monsoon and usually maximum activity late in the summ
er (southwest) monsoon.