Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 4; Volume 8, Part 4American Society of Mechanical Engineers, 1989 - Arctic regions |
From inside the book
Results 1-3 of 82
Page 199
... iceberg . The motion of the iceberg in the negative F2 direction ( Figure 1c ) is consistent with the initial orientation of the iceberg . The translational motions in this and other simulations result from the horizontal components of ...
... iceberg . The motion of the iceberg in the negative F2 direction ( Figure 1c ) is consistent with the initial orientation of the iceberg . The translational motions in this and other simulations result from the horizontal components of ...
Page 201
notch results in the iceberg attaining its equilibrium position in a time slightly less than that for the iceberg in Figure 2. The reduced mass may also have contributed to the changes in the time to attain equilibrium . A detailed ...
notch results in the iceberg attaining its equilibrium position in a time slightly less than that for the iceberg in Figure 2. The reduced mass may also have contributed to the changes in the time to attain equilibrium . A detailed ...
Page 296
... iceberg during a given period of time . As proposed by Dunwoody [ 2 ] , input probability distributions for iceberg mass and drift veloc- ity must be modified to account for the increased likelihood of larger and faster icebergs ...
... iceberg during a given period of time . As proposed by Dunwoody [ 2 ] , input probability distributions for iceberg mass and drift veloc- ity must be modified to account for the increased likelihood of larger and faster icebergs ...
Contents
OFFSHORE MECHANICS | 1 |
The Growth of Radial Cracks in Ice Sheets | 7 |
ICE FORCES | 11 |
Copyright | |
30 other sections not shown
Other editions - View all
Common terms and phrases
analysis angle Arctic Engineering assumed Barents Sea Beaufort Sea behaviour berm Bjørnøya calculated coefficient Cole components computed Conference on Offshore constant constitutive equation damage evolution damage model deformation density depth determined diameter distribution dynamic effect energy equation experimental factor failure force fracture mechanics fracture toughness frequency friction function Geogrid grain horizontal ice floe ice load ice sheet ice thickness iceberg icebreaking impact increase indentor initial interaction keel material maximum measured Mechanics and Arctic Mellor microcracks modulus motion notch nucleation observed obtained ocean Offshore Mechanics parameters peak stress plane polycrystalline ice predicted pressure probability Proc radar ratio resistance ridge samples sea ice seabed shear shear stress ship shown in Figure simulation specimen spray ice strain rate strain tensor strength structure surface temperature tensile tensile stress tensor tests uniaxial compression variable vector velocity vertical wave Young's modulus