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- W4243504003 abstract "ON the coasts of the British Islands and generally on the European coasts of the North Atlantic and throughout the North Sea, the tides present in their main features an exceptional simplicity, two almost equally high high-waters and two almost equally low low-waters in the twenty-four hours, with the regular fortnightly inequality of spring tides and neap tides due to the alternately conspiring and opposing actions of the moon and sun, and with large irregular variations produced by wind. Careful observation detects a small “diurnal” inequality, (so called because it is due to tidal constituents having periods approximately equal to twenty-four hours lunar or solar) of which the most obvious manifestation is a difference at certain times of the month and of the year between the heights of the two high-waters of the twenty-four hours, and at intermediate times a difference between the heights of the two low-waters." @default.
- W4243504003 created "2022-05-12" @default.
- W4243504003 date "1878-10-01" @default.
- W4243504003 modified "2023-09-26" @default.
- W4243504003 title "ON THE TIDES OF THE SOUTHERN HEMISPHERE AND OF THE MEDITERRANEAN 1" @default.
- W4243504003 doi "https://doi.org/10.1038/018670a0" @default.
- W4243504003 hasPublicationYear "1878" @default.
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