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Geoscience Letters

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
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