323 



11 





II. Discussion of the Preceding Results. 

 The tides seem to be normal for a place in the Southern Ocean. The semi-diurnal tides are considerable, 

 but the solar tide is unusually large compared with the lunar tide, the ratio being i, or 0-6, as compared' 

 Vith 0-465 of the equilibrium theory. The semi-diurnal tides are almost exactly "inverted," so that low 

 water occiu-s very nearly when the moon is on the meridian. 



