Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 7, Parts 4-6American Society of Mechanical Engineers, 1988 - Arctic regions |
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Page 72
... layer . Since the water drag at the bottom of the mixed layer is zero , we must remove the surface elevation satisfies variations in the mixed incompressibility restraint . term from ( 12 ) . The ( neglecting thickness layer ) the usual ...
... layer . Since the water drag at the bottom of the mixed layer is zero , we must remove the surface elevation satisfies variations in the mixed incompressibility restraint . term from ( 12 ) . The ( neglecting thickness layer ) the usual ...
Page 94
... layer . This allows two import- ant simplications : ( 1 ) stress in the surface layer is assumed constant , and ( 2 ) wind ( analogous to current measured with respect to the drifting ice ) and stress are assumed col- linear . Tennekes ...
... layer . This allows two import- ant simplications : ( 1 ) stress in the surface layer is assumed constant , and ( 2 ) wind ( analogous to current measured with respect to the drifting ice ) and stress are assumed col- linear . Tennekes ...
Page 113
... layer thickness , varying as function of 0 , and vo velocity of the indenter . Figure 3 , a varying layer thickness is illustrated ; other patterns are possible , for example with the thickness increasing from the axis of symmetry to ...
... layer thickness , varying as function of 0 , and vo velocity of the indenter . Figure 3 , a varying layer thickness is illustrated ; other patterns are possible , for example with the thickness increasing from the axis of symmetry to ...
Contents
ICE PROPERTIESII | 31 |
Simple Beam Tests on Type S3 Sea | 63 |
ICE DRIFT AND DYNAMICS | 69 |
Copyright | |
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analysis angle approximately Arctic assumed average beam calculated coefficient Cold conducted Conference constant crack creep crushing curves deflection deformation dependence determined developed drift dynamic effect elastic energy Engineering equation estimated experimental experiments factor failure field Figure flexural flow force fracture friction function given grain heat horizontal ice force ice loads ice sheet iceberg impact increase indicates International island layer length limit linear material mean measured Mechanics method motion normal Norton Sound observed obtained Ocean Offshore operating oriented panel parameters plate POSITION presented pressure properties range ratio reference region reinforced relative Report Research response saline samples scale sea ice shape ship shown shows specimen speed spray strain rate strength stress structure surface Table temperature tests thermosyphon thickness tion transfer values vertical wind