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Directional Recording of Swell from Distant Storms - Department of ...

Directional Recording of Swell from Distant Storms - Department of ...

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DIRECTIONAL RECORDING OF SWELL FROM DISTANT STORMS 565turn modulates the vibration transducer (1 04 c/s) whose output modulates the radio transmitter(108 c/s). An analysis <strong>of</strong> successive 3 h records failed to show such an effect. Thisprovides an upper limit on the velocity <strong>of</strong> the near-shore tidal currents. A tidal frequencymodulation above one part in 300 could have been detected. The tidal currents are thenless than 1/300 <strong>of</strong> the phase velocity, or less than W knot.13. GENERATION AND DECAY(a) Ridge cutsFigure 40 shows the variation in energy density with frequency along some <strong>of</strong> the ridgesin thef-t diagrams. The significance <strong>of</strong> the 'ridge cut' is that the effect <strong>of</strong> dispersion isremoved, so that we can infer the spectrum in the source area as modified by attenuationalong the path.60 kNOTS.8 9 m 50 KNOTS.Ct42~~~~~~~~~~~~~~~~~~~~~~~~~~~-_w ~~~~~~~~~~~_,~ E 40 KNOX100GAS~ ~ ~~~~~~~~~r\ r * A15? 20S? 8250T0*001 !7/ /I I _ _ I I I0 10 20 30 40 50 60 70 80 90 100C/KSFIGURE 40. The curves marked 30, 40, 50, 60 knots are Darbyshire's empirical spectra in the generationarea. The associated root-mean-square heights (crest-to-trough) are entered. For comparison,the variation <strong>of</strong> energy density with frequency along four well-developed ridges is shown;time, distance and direction, as entered, are those determined <strong>from</strong> the wave observrations. Thewind speed in knots is taken <strong>from</strong>n the weather maps. The dots mark the ' cut-<strong>of</strong>f points ': to theleft the measured E(f) values are in reasonable accord with the empirical curves, to the rightthey fall below the empirical curves,- presumably because <strong>of</strong> attenuation. The open circlesrefer to the northern sources <strong>of</strong> 8-9 and 23'2 October, the remaining circles to all other events.The characteristic feature is the very sharp cut-<strong>of</strong>f <strong>of</strong> the low-frequency side <strong>of</strong> the wavespectra. The energy diminishes by a factor 200:1 between 50 and 40 c/ks, or at a rate <strong>of</strong>100 db's per octave. Waves in the generating area- similarily show a sharp low-frequencycut-<strong>of</strong>f, so sharp that there has been difficulty in resolving it. In fact the suggestion has beenmade by Phillips (personal communication) that a discontinuous functionE(f>~f5 for f>f*; E(f)-0 for f

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