Show tidal though alig cicat cht and most ie art frt lining to tre of tl 0 aca is ho tidal rei utilio authorities that it still p some ui axi lun ablo abom alecs it is demonstrated 1 tl at alio movement 13 undo up cf leou lent upon fund eions of the and bun shiao being diurnal amsi tl 0 and uio eccli nation of both bo lies croato great iari etious rho cl ce an 11 asi lion of tl e and alie position of her no lo 10 also laio o effect tl 0 mer viru direction aul dorco of ho vinda aid tho ot alio ero pla their lart au ewt m this acla tiou is that observations all over the world bl ow no pl ico v ero tl 0 ti lal movement is fo regular aud aa aroun 1 tho ii a fact more rem when it is th it the tho other si ie of the atlantic as for instance at ioa facomia ire very complicated the ui explainable case 1 ero being tl at tho minor in moot parts of bo world when combined in one direction amount to a ery fraction of capal lunar and solar tides an 1 ono greatly increase or their effects are in great britain so in significant that their is tn fling lew york sun |