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Official Journal of the Asia Oceania Geosciences Society (AOGS)

Table 1 Amplitudes H and phase lags G of tidal components

From: A fortnightly atmospheric ‘tide’ at Bali caused by oceanic tidal mixing in Lombok Strait

Tide Argument Frequency (\(^{\circ}/\mathrm {h}\)) SST at (\(9^{\circ}\mathrm{{S}}\), \(115.5^{\circ}\mathrm{{E}}\)) Bali air temp. Bali rel. humidity
H G H G H G
MSfa 2s–3h 0.97483 49 ± 25 183 ± 30 80 ± 19 171 ± 14 0.36 ± 0.10 351 ± 17
MSf 2s–2h 1.01590 143 ± 25 322 ± 10 66 ± 19 290 ± 16 0.49 ± 0.10 99 ± 12
MSfb 2s–h 1.05696 80 ± 25 90 ± 18 62 ± 19 54 ± 18 0.42 ± 0.10 231 ± 14
  1. Amplitude units: mK for temperatures, percent for relative humidity. Phase lag units: degrees