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The wind field over wind-waves
Journal of the Oceanographical Society of Japan, 1976The velocity fluctuations of wind over wind-waves in a wind tunnel are measured with a X-type hot-wire anemometer at some heights over the water surface.
Hiroshi Ichikawa, Norihisa Imasato
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BERNSTEIN WAVES IN THE SOLAR WIND
1992Pronounced emission peaks at a series of frequencies in the electron cyclotron harmonic (ECH) frequency range, observed at a lithium neutralgas release in the solar wind, are interpreted in terms of Bernstein waves (electrostatic waves in the ECH frequency range propagating perpendicular to the ambient magnetic field). The observed distinct frequencies
Baumgärtel, K., Sauer, K.
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Strong Coupling of Wind and Wind Waves
1992Observational evidence is presented that the wind and the wind waves are in strong coupling in their fluctuations. In this strong coupling the wave breaking should play an essential role. A 4.5-hour time series of wind profile and wind-wave statistics, obtained at an oceanographic tower station under a winter monsoon wind, were reanalyzed.
Y. Toba, H. Kawamura, N. Ebuchi
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Proceedings of the European Wave and Tidal Energy Conference
Wave Dragon wave-wind project Wave power is more consistent than wind-, solar- and tidal power. Wave is at the same time more predictable than wind and solar. The paper assesses the economic performance of the different wave energy converter (WEC) types and discusses the possibility for WECs to match the levelized cost of energy for offshore wind ...
Erik Friis-Madsen +4 more
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Wave Dragon wave-wind project Wave power is more consistent than wind-, solar- and tidal power. Wave is at the same time more predictable than wind and solar. The paper assesses the economic performance of the different wave energy converter (WEC) types and discusses the possibility for WECs to match the levelized cost of energy for offshore wind ...
Erik Friis-Madsen +4 more
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Duality of turbulence and wave in wind waves
Journal of the Oceanographical Society of Japan, 1974The three-seconds power law for wind waves of simple spectra, already derived byToba (1972 and 1973), may also be derived by introducing surface-wave properties into the form of the rate of energy dissipation in the theory of turbulence. The universal constantB, which was formerly determined empirically as 0.062 is here obtained asB=(2π)−3/2=0.0635 ...
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Extreme Wind and Waves in U.S. East Coast Offshore Wind Energy Lease Areas
Energies, 2021Frederick Letson +2 more
exaly