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Depth variation of energy transport in fluid gravity waves
We calculate the distribution of energy flux as a function of the distance below the surface for propagating polychromatic gravity fluid surface waves. Linear theory has been used to derive closed-form expressions for the energy flux as a function of depth. In this context we discuss the power distribution for real ocean waves measured off the west coast of Sweden and compare this to the energy flux distribution for waves with Pierson–Moskowitz and Bretschneider spectral distributions. This is done in order to get an improved understanding of how to improve the power absorption in wave energy converters, and this is also discussed in this paper.
Depth variation of energy transport in fluid gravity waves
We calculate the distribution of energy flux as a function of the distance below the surface for propagating polychromatic gravity fluid surface waves. Linear theory has been used to derive closed-form expressions for the energy flux as a function of depth. In this context we discuss the power distribution for real ocean waves measured off the west coast of Sweden and compare this to the energy flux distribution for waves with Pierson–Moskowitz and Bretschneider spectral distributions. This is done in order to get an improved understanding of how to improve the power absorption in wave energy converters, and this is also discussed in this paper.
Depth variation of energy transport in fluid gravity waves
Isberg, Jan (Autor:in) / Engstro¨m, Jens (Autor:in) / Leijon, Mats (Autor:in)
Journal of Renewable and Sustainable Energy ; 2 ; 023104-
01.03.2010
10 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Englisch
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