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- W4231526122 abstract "THE tidal oscillation of the ocean may be represented as the sum of a number of simple harmonic waves which go through their periods approximately once, twice, thrice, four times in a mean solar day. But these simple harmonic waves may be regarded as being rigorously diurnal, semi-diurnal, terdiurnal, and so forth, if the length of the day referred to be adapted to suit the particular wave under consideration. The idea of a series of special scales of time is thus introduced, each time-scale being appropriate to a special tide. For example, the mean interval between successive culminations of the moon is 24h. 50m., and this interval may be described as the mean lunar day. Now there is a series of tides, bearing the initials M1, M2, M3, M4, &c., which go through their periods rigorously once, twice, thrice, four times, &c., in a mean lunar day. The solar tides, S, proceed according to mean solar time, but, besides mean lunar and mean solar times, there are other special time scales appropriate to the other tides." @default.
- W4231526122 created "2022-05-12" @default.
- W4231526122 date "1893-02-01" @default.
- W4231526122 modified "2023-09-27" @default.
- W4231526122 title "Reduction of Tidal Observations" @default.
- W4231526122 doi "https://doi.org/10.1038/047402a0" @default.
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