Cartesian diver observations of double frequency pressure fluctuations in the upper levels of the ocean
Pressure oscillations having a narrow spectrum centered at 0.175 Hz have been measured in the deep sea at depths between 100 and 300 m. At these depths the nonlinear interaction between oppositely directed sea surface gravity waves causes pressure fluctuations, the intensity of which varies inversel...
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Veröffentlicht in: | Geophysical research letters 1989-08, Vol.16 (8), p.807-810 |
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