Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 2American Society of Mechanical Engineers, 2006 - Arctic regions |
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Page 395
... velocity , um , and the time elapsed between two successive zerocrossing points , The . A new relationship for the wake velocity and a numerical procedure for describing the time history of CD ( t ) and C1 ( t ) are introduced . A ...
... velocity , um , and the time elapsed between two successive zerocrossing points , The . A new relationship for the wake velocity and a numerical procedure for describing the time history of CD ( t ) and C1 ( t ) are introduced . A ...
Page 443
... velocity distribution model was derived and compared with the traditional logarithmic model . It should be pointed out that the velocity data adopted have four layers within one meter above the bed , and the roughness length z , is ...
... velocity distribution model was derived and compared with the traditional logarithmic model . It should be pointed out that the velocity data adopted have four layers within one meter above the bed , and the roughness length z , is ...
Page 601
... Velocity ( m / s ) Velocity ( m / s ) ( Viscous ) ( Inviscid ) Horizontal - Maximum 9.58E - 03 1.60E - 02 Minimum -4.10E - 02 -3.52E - 02 Mean -1.64E - 02 -1.02E - 02 8 85 9 95 10 Vertical - Maximum 7.40E - 04 8.87E - 04 Time ( s ) ...
... Velocity ( m / s ) Velocity ( m / s ) ( Viscous ) ( Inviscid ) Horizontal - Maximum 9.58E - 03 1.60E - 02 Minimum -4.10E - 02 -3.52E - 02 Mean -1.64E - 02 -1.02E - 02 8 85 9 95 10 Vertical - Maximum 7.40E - 04 8.87E - 04 Time ( s ) ...
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