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 83
... ocean interaction at high latitude . Thermally gener- ated surface winds , blowing from ice to water ( ice breeze ) with some deflection due to the earth rotation , force the ice drift and ocean currents near the MIZ . By changing the ...
... ocean interaction at high latitude . Thermally gener- ated surface winds , blowing from ice to water ( ice breeze ) with some deflection due to the earth rotation , force the ice drift and ocean currents near the MIZ . By changing the ...
Page 89
... ocean coupled model is intended to depict only the mesoscale process- es of air - ice - ocean interactions in the MIZ . The synoptic scale pressure gradient may addi- tionally produce surface winds in the MIZ , and large - scale ocean ...
... ocean coupled model is intended to depict only the mesoscale process- es of air - ice - ocean interactions in the MIZ . The synoptic scale pressure gradient may addi- tionally produce surface winds in the MIZ , and large - scale ocean ...
Page 100
... ocean and when advected with the Atlantic water they will eventually interact with the ice and polar water . Atmospheric interactions , ice growth , and surface gravity waves are most intense from about December to April . Annually ...
... ocean and when advected with the Atlantic water they will eventually interact with the ice and polar water . Atmospheric interactions , ice growth , and surface gravity waves are most intense from about December to April . Annually ...
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