Abstract A harmonic-analysis technique is used to compute tidal amplitudes and phases over the south-west Pacific Ocean from the first 300 cycles (up to November 2000) of TOPEX/Poseidon satellite altimetry. The analysis is performed along groundtracks and at track crossover locations and the resultant harmonics are shown to compare favourably with those from open-coast sea-level gauges and from regional and global tidal models. Small-scale oscillations (<400 km) in along-track amplitudes and phases are used to identify likely regions of M2 internal tide generation, or aliasing between K1 and semi-annual signals. Tidal harmonics derived from satellite altimetry were used to improve the open-sea boundary forcing for a limited-area tidal model and produce a better validation with coastal sea-level gauges.
Keywords satellite altimetry; TOPEX/Poseidon; tides; internal tides; model; South Pacific Ocean
M03023; Received 9 May 2003; accepted 12 May 2004; Online publication date
5 August 2004
New Zealand Journal of Marine and Freshwater Research, 2004, Vol. 38:
649-669
0028-8330/04/3804-0649 © The Royal Society of New Zealand 2004
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