Fig. 4
From: A fortnightly atmospheric ‘tide’ at Bali caused by oceanic tidal mixing in Lombok Strait
MSf phase lags, i.e., times within a spring–neap cycle of (top to bottom): maximum relative humidity at Bali; minimum air temperature at Bali; minimum SST in a region surrounding Lombok Strait; maximum tidal current speeds within Lombok Strait; and maximum spring-tide elevations at the Benoa tide gauge. Uncertainties represent \(\pm 2\sigma\). The tidal semidiurnal currents are extracted from the barotropic finite-element model FES2014 (updated Lyard et al. 2006), which are drawn out explicitly in the lower panel