Nineteen years of hourly tide readings at Honolulu, Hawaii, and Newlyn, England, are analysed without astronomical prejudice as to what frequencies are present, and what are not, thus allowing for background noise. The method consists of generating various complex input functions c _i , ( t ) for the same time interval as the recorded tide £( t ), and of determining the associated lag weights w in the convolutions

\hat{ζ} (t) = \sum_{i} \sum_{S} w_{i s} c_{i} (t - τ_{s}) + \sum_{i j} \sum_{s s^{'}} w_{i j s s^{'}} c_{i} (t - τ_{s}) c_{j} (t - τ_{s^{'}}) + . . .

by the condition ((£—£)2) = minimum. The two expansions represent linear and bilinear processes; the Fourier transforms of w for any chosen i (or ij ) are the linear (or bilinear) admittances. Input functions are the (time variable) spherical harmonics of the gravitational potential and of radiant flux on the Earth’s surface; these functions are numerically generated hour by hour, directly from the Kepler-Newton laws and the known orbital constants of Moon and Sun, without time-harmonic expansions (unlike the harmonic method of Kelvin-Darwin-Doodson). The radiative input is required to predict non-gravitational tides, and it allows for the essential distinction that the Earth is opaque to radiation and transparent to gravitation.

Tidal Resonance in the Coral Sea

Abstract

Keywords