Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 4American Society of Mechanical Engineers, 1988 - Arctic regions |
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Page 93
... flow at one location into separate realizations assuming that spatial variation is advected past the probe with the mean flow . Turbulent statis- tics are calculated for each realization , with mean vector and tensor quantities rotated ...
... flow at one location into separate realizations assuming that spatial variation is advected past the probe with the mean flow . Turbulent statis- tics are calculated for each realization , with mean vector and tensor quantities rotated ...
Page 291
... flow inside the evaporator tubes . To accommodate this it is necessary to recognize that flow takes place only during the period when the feed pump exhaust valve is open : that is , for about 80 degrees . If this " pulse " is ...
... flow inside the evaporator tubes . To accommodate this it is necessary to recognize that flow takes place only during the period when the feed pump exhaust valve is open : that is , for about 80 degrees . If this " pulse " is ...
Page 304
... flow is more stable . It is also seen that , for larger values of R , the flow is less stable . This is because as R increases , the buoyancy force increases . Since the buoyancy force is the destabilized factor , therefore the flow is ...
... flow is more stable . It is also seen that , for larger values of R , the flow is less stable . This is because as R increases , the buoyancy force increases . Since the buoyancy force is the destabilized factor , therefore the flow is ...
Contents
OFFSHORE MECHANICS | 1 |
The Structure and Tensile Behavior of First Year Sea Ice and LaboratoryGrown Saline | 11 |
Effects of Temperature and Strain Rate on Uniaxial Compressive Strength of Naturally Formed Fresh | 19 |
Copyright | |
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analysis Arctic Arctic Engineering average beam Beaufort Sea Bering Sea buoys caisson compressive crack creep curves deflection deformation delayed elastic density diameter dome drift dynamic effect EGADS energy equation estimate experimental factor failure flexural strength floe fracture toughness freshwater ice friction coefficient gauges geostrophic wind horizontal ice drift ice edge ice force ice loads ice motion ice pressure ice sheet ice tests ice thickness ice velocity iceberg icebreaking impact increase indentation interaction island layer linear measured Mechanics and Arctic method MIZEX model ice model tests modulus Molikpaq normal force ocean Offshore Mechanics parameters peak pressure panel PVDF ratio reinforced ice Research saline samples scale sea ice sediments shear shear strength ship shown in Figure Sinha specimen speed spray ice strain gauges strain rate stress structure surface temperature tensor thermosyphon Timco tion uniaxial values vertical wind