Official Journal of the Asia Oceania Geosciences Society (AOGS)
Table 2 Amplitudes and Greenwich phase lags of major ocean tides at Benoa Harbor
From: A fortnightly atmospheric ‘tide’ at Bali caused by oceanic tidal mixing in Lombok Strait
Tide | Amplitude (mm) | Phase |
|---|---|---|
Sa | 150 | \(330^{\circ}\) |
Ssa | 61 | \(167^{\circ}\) |
\(\mathrm {O}_1\) | 162 | \(156^{\circ}\) |
\(\mathrm {P}_1\) | 73 | \(173^{\circ}\) |
\(\mathrm {K}_1\) | 253 | \(177^{\circ}\) |
\(\mathrm {N}_2\) | 114 | \(28^{\circ}\) |
\(\mathrm {M}_2\) | 642 | \(53^{\circ}\) |
\(\mathrm {S}_2\) | 367 | \(108^{\circ}\) |
\(\mathrm {K}_2\) | 102 | \(106^{\circ}\) |