Fig. 5
From: A fortnightly atmospheric ‘tide’ at Bali caused by oceanic tidal mixing in Lombok Strait
Seasonal variations of the fortnightly oscillations in SST south of Lombok Strait and in Bali air temperature and Bali relative humidity. The dotted lines delineate the seasonal envelope of the fortnightly signals; these envelopes are evaluated from \(\widetilde{H},\widetilde{G}\) of Eq. (5), with constants from Table 1. The fortnightly signals all peak during boreal summer