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 69
... ice speed was 87cm / s near the Bering Strait . Free - drift ice models showed that the ice velocity could be decomposed into ( i ) locally wind - driven ice velocity relative to the current beneath the mixed layer , and ( ii ) current ...
... ice speed was 87cm / s near the Bering Strait . Free - drift ice models showed that the ice velocity could be decomposed into ( i ) locally wind - driven ice velocity relative to the current beneath the mixed layer , and ( ii ) current ...
Page 73
... Ice Velocity onto Wind ( V - W ) , Ice Velocity onto Current ( V - C ) , Current onto Wind ( C - W ) , and Relative Current onto Wind ( R - W ) . The parameters result from fitting y = Ax + B , where A – aexp ( in ) and B = brtibi , oy2 ...
... Ice Velocity onto Wind ( V - W ) , Ice Velocity onto Current ( V - C ) , Current onto Wind ( C - W ) , and Relative Current onto Wind ( R - W ) . The parameters result from fitting y = Ax + B , where A – aexp ( in ) and B = brtibi , oy2 ...
Page 75
... velocity are estimated for the region between Fram Strait and the North Pole . Spatial varia- tions in these statistics , and in the response of the ice velocity to concurrent ... Ice Motion, Fram Strait to North Pole R E Moritz and R Colony.
... velocity are estimated for the region between Fram Strait and the North Pole . Spatial varia- tions in these statistics , and in the response of the ice velocity to concurrent ... Ice Motion, Fram Strait to North Pole R E Moritz and R Colony.
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 angle approximately Arctic assumed average beam boundary calculated coefficient Cold conducted Conference constant crack creep crushing curves deflection deformation dependence described determined developed direction drift dynamic effect elastic energy Engineering equation estimate experimental experiments factor failure field Figure flexural flow fracture friction function given grain heat horizontal ice force ice loads ice sheet ice velocity iceberg impact increase indentation indicates International island layer length limit linear material mean measured Mechanics method motion Norton Sound observed obtained ocean Offshore operating oriented parameters POSITION presented pressure properties range ratio reference region relative Report Research response saline samples scale sea ice shape ship shown shows specimen speed strain rate strength stress structure surface Table temperature tests theory thickness tion values variations vertical wind