Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 2American Society of Mechanical Engineers, 2001 - Arctic regions |
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Page 218
( 1973 ) proposed the JONSWAP spectrum that described fetch - limited waves very well using £ ve parameters ( fp , Oj , Yj , 0 , and ob ) : 5 v - fp ) 20217 4 - ( -36 ) SV ) = Qjg ? 21 ) -48-5 exp exp Y 1931,5l ) ( 1 ) plitude of ...
( 1973 ) proposed the JONSWAP spectrum that described fetch - limited waves very well using £ ve parameters ( fp , Oj , Yj , 0 , and ob ) : 5 v - fp ) 20217 4 - ( -36 ) SV ) = Qjg ? 21 ) -48-5 exp exp Y 1931,5l ) ( 1 ) plitude of ...
Page 224
Kitaigorodskii , S. A. , On the Theory of the Equilibrium Range in the Spectrum of Wind - Generated Gravity Waves , Journal of Physical Oceanography , 13 , 816-827 , 1983 . Kitaigorodskii , S. A. , Applications of the Theory of ...
Kitaigorodskii , S. A. , On the Theory of the Equilibrium Range in the Spectrum of Wind - Generated Gravity Waves , Journal of Physical Oceanography , 13 , 816-827 , 1983 . Kitaigorodskii , S. A. , Applications of the Theory of ...
Page 395
S ( w + Aw ) . dw 2 Sw Sow The response spectrum of the system motion is then : SR ( AW ) = 2 R2 ( AW ) . SQTF ( W , Aw ) . S ( W ) . Sw + Aw ) . do where R is the transfer function of the system that , in first approximation , can be ...
S ( w + Aw ) . dw 2 Sw Sow The response spectrum of the system motion is then : SR ( AW ) = 2 R2 ( AW ) . SQTF ( W , Aw ) . S ( W ) . Sw + Aw ) . do where R is the transfer function of the system that , in first approximation , can be ...
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