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 20
also satisfy the boundary conditions at the free surface . The first order surface is linear in the sense that the individual sinusoids can be added together to describe a directionally spread and dispersive surface . Once the waves ...
also satisfy the boundary conditions at the free surface . The first order surface is linear in the sense that the individual sinusoids can be added together to describe a directionally spread and dispersive surface . Once the waves ...
Page 22
... surface , gives velocities which are too small . The HWM appears to be quite accurate . Zhang ( 1999b ) have also ... free surface can be calculated from a similar transformation . Estimates of the horizontal and vertical velocities on ...
... surface , gives velocities which are too small . The HWM appears to be quite accurate . Zhang ( 1999b ) have also ... free surface can be calculated from a similar transformation . Estimates of the horizontal and vertical velocities on ...
Page 23
... free surface boundary conditions can be written in the form ( a ) η , = - Φι - Ψηφ = { 1Vq12 – 8n - ( 6 ) ( 7 ) Horizontal Velocity , u [ m / s ] 0.4 0.2 · -0.2 Vertical Velocity , v [ m / s ] 7 0.4 0.2 · -0.2 ) -2 -3 -2 -1 ( c ) 2 3 ...
... free surface boundary conditions can be written in the form ( a ) η , = - Φι - Ψηφ = { 1Vq12 – 8n - ( 6 ) ( 7 ) Horizontal Velocity , u [ m / s ] 0.4 0.2 · -0.2 Vertical Velocity , v [ m / s ] 7 0.4 0.2 · -0.2 ) -2 -3 -2 -1 ( c ) 2 3 ...
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