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Simulation of Velocity Profile under Ice Cover

World Environmental and Water Resource Congress 2006, 2006
Based on a k- model and using a finite volume method, a model was developed to simulate the 2-dimensional velocity profile under ice cover. The comparison of the simulated results from this model with the measured data from experiments indicated that the data matched well with each other.
Jun Wang   +3 more
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Ejection velocities of ice fragments in oblique impacts of ice spheres

Advances in Space Research, 1999
Reaccumulation conditions of icy planetesimals in collisional disruption were studied experimentally using a one-stage light gas gun set in a cold room (−18°C). Oblique impacts between ice spheres were used to measure the velocity distributions of fragments. The impact velocities ranged from 170 to 640 m/s, and the projectile-to-target mass ratio was a
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Velocity Effects on Conical Structure Ice Loads

21st International Conference on Offshore Mechanics and Arctic Engineering, Volume 3, 2002
Existing design codes and most methods for ice load calculation for conical structures do not take velocity effects into account. They were developed as an upper bound estimate for the load from slow moving ice which fails in bending against the cone. Velocity effects can be ignored when the structure is designed for an area with slow ice movement, for
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Velocity of Sliding of an Ice-fall

Nature, 1963
DURING the Nepal Himalaya P-29 (7,835m) Expedition of Osaka University Mountaineering Club, 1961, we had some experience on sliding and avalanches of an active ice-fall; analysing photographs taken by a Canon 2,000mm telephotographic lens from the base camp at 4,400 m high. Fig. 1 is a series of photographs taken at: (a) May 10, 1° 30′ p.m.; (b) May 11,
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Glacier Ice Surface Velocity Using Interferometry

2023
M. Geetha Priya   +2 more
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Kink velocities on dislocations in ice

Philosophical Magazine, 1976
H. J. Frost, D. J. Goodman, M. F. Ashby
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Maximum Velocity of Ice Boats

Scientific American, 1880
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The Velocity of Ice Boats

Scientific American, 1880
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