Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 18, Part 5American Society of Mechanical Engineers, 1999 - Arctic regions |
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Page 172
... that is , the general solution satisfies the governing equation and associated boundary conditions except that on the structure surface . The boundary expansion method proposed by one of authors is then introduced for how ...
... that is , the general solution satisfies the governing equation and associated boundary conditions except that on the structure surface . The boundary expansion method proposed by one of authors is then introduced for how ...
Page 347
The results are valid for unstratified planetary boundary layer flow and are based on similarity theory . The geostrophic drag coefficient and the direction of the surface shear stress are presented for steady flow conditions .
The results are valid for unstratified planetary boundary layer flow and are based on similarity theory . The geostrophic drag coefficient and the direction of the surface shear stress are presented for steady flow conditions .
Page 353
Soulsby , R.L. , 1983 , “ The bottom boundary layer of shelf seas ” , Physical Oceanography of Coastal and Shelf Seas , ed . , B. Johns , Elsevier , New York , pp . 189-266 . Soulsby , R.L. , 1990 , “ Tidal - current boundary layers ” .
Soulsby , R.L. , 1983 , “ The bottom boundary layer of shelf seas ” , Physical Oceanography of Coastal and Shelf Seas , ed . , B. Johns , Elsevier , New York , pp . 189-266 . Soulsby , R.L. , 1990 , “ Tidal - current boundary layers ” .
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Contents
OMAE99PA1135 | 19 |
OMAE99PA1141 | 39 |
PROPELLERICE INTERACTION | 53 |
Copyright | |
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