Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 11, Part 4American Society of Mechanical Engineers, 1992 - Arctic regions |
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Page 54
the ambient temperature decreases across other lower temperature boundaries . Decreasing the ambient temperature from -5 ° C to -15 ° C does not produce the same proportionate benefits as decreasing the ambient temperature from -15 ° C ...
the ambient temperature decreases across other lower temperature boundaries . Decreasing the ambient temperature from -5 ° C to -15 ° C does not produce the same proportionate benefits as decreasing the ambient temperature from -15 ° C ...
Page 114
... temperature data are usually available from published weather records or environmental atlases . However , very few long - term ground surface temperature data have been collected . As a result , an empirical approach has been developed ...
... temperature data are usually available from published weather records or environmental atlases . However , very few long - term ground surface temperature data have been collected . As a result , an empirical approach has been developed ...
Page 132
... temperature causes a layer of the soil to freeze and thaw as the temperature fluctuates around the freezing temperature of water ( 0 ° C ) . Since the properties of frozen and thawed soils are significantly different , the study of this ...
... temperature causes a layer of the soil to freeze and thaw as the temperature fluctuates around the freezing temperature of water ( 0 ° C ) . Since the properties of frozen and thawed soils are significantly different , the study of this ...
Contents
ICEENVIRONMENT STATISTICS | 1 |
Seasonal Ice Cover Variability in a Coupled IceOcean Model for the Arctic Ocean | 11 |
An Illustration of Theoretical and Empirical Errors and the Effect of the Resolution of the | 21 |
Copyright | |
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analysis angle Arctic/Polar Technology ASME beam Beaufort Sea berm brine calculated Canada Cold Regions compressive conducted crack creep Croasdale curves deflection density displacement drag drag coefficient effect elastic equation evaporator experimental failure finite element flexural floe flow fluid form drag fracture toughness freezing frequency friction coefficient heat transfer ice cover ice forces ice load ice movement ice plates ice rubble ice sheet ice thickness increase indentor Laboratory layer length linear maximum mode offshore structure OMAE panels parameters permafrost pile plane strain plastic Plastic Analysis plotted Poisson's Ratio pore pressure predictions ratio Research Ride-Up ridge rubble field salinity samples scale sea ice sensors shear shear strength shear stress shown in Figure simulation snow soil spray ice strain rate strength stress surface Technology ASME 1992 temperature thaw thaw depth thermal thermosyphon Timco tube Tuktoyaktuk values velocity vertical