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 Arctic Engineering average beam Beaufort Sea Bering Sea buckling buoys Cold Regions compressive Conference on Offshore crack creep crushing curves deflection deformation density diameter drift dynamic effect elastic modulus equation estimated experimental factor failure flexural strength floe fracture toughness freshwater ice friction coefficient gauges geostrophic wind grain heat transfer horizontal ice drift ice force ice loads ice motion ice pressure ice sheet ice tests ice thickness ice velocity iceberg icebreaking impact increase indentation island layer linear measured Mechanics and Arctic method MIZEX model ice modulus Molikpaq normal force Norton Sound Ocean Offshore Mechanics oriented parameters pressure panel PVDF ratio reinforced ice Research samples scale sea ice sediments shear ship shown in Figure Sinha Sodhi specimen spray ice strain gauges strain rate strain tensor structure surface temperature tensor thermosyphon Timco tion uniaxial values vertical