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• Mass Loading Model of Ice
  ...ng ocean waves by shore-fast sea ice, modelled by a semi-infinite sheet of ice. The first attempt at a solution was by [[Weitz and Keller 1950]] who solve ...om five to one, eliminating the need to apply additional conditions at the ice-edge.
  2 KB (279 words) - 01:38, 17 February 2010
• Ice as a Thin Elastic Plate
  ...problems. (Another noteworthy comment that was made in that paper is that ice was the first material for which an experimental value of Young's modulus w ...de the compressibility of the water beneath the ice sheet and to model the ice as a thin plate rather than as a beam (i.e. as a three-dimensional structu
  6 KB (981 words) - 01:41, 17 February 2010
• Category:Wave Scattering in the Marginal Ice Zone
  The marginal ice zone (MIZ) is an interfacial region that forms at the boundary of the or frozen ocean, consisting of a patchwork of ice floes and open water. Wave processes are very
  4 members (0 subcategories, 0 files) - 01:44, 17 February 2010

Page text matches

• Shen and Squire 1998
  ...re, Wave damping in compact pancake ice fields due to interactions between ice cakes,
  175 bytes (24 words) - 01:47, 17 February 2010
• Mass Loading Model of Ice
  ...ng ocean waves by shore-fast sea ice, modelled by a semi-infinite sheet of ice. The first attempt at a solution was by [[Weitz and Keller 1950]] who solve ...om five to one, eliminating the need to apply additional conditions at the ice-edge.
  2 KB (279 words) - 01:38, 17 February 2010
• Press and Ewing 1951
  F Press, M Ewing, Propagation of elastic waves in a floating ice sheet,
  132 bytes (19 words) - 01:40, 17 February 2010
• Ice as a Thin Elastic Plate
  ...problems. (Another noteworthy comment that was made in that paper is that ice was the first material for which an experimental value of Young's modulus w ...de the compressibility of the water beneath the ice sheet and to model the ice as a thin plate rather than as a beam (i.e. as a three-dimensional structu
  6 KB (981 words) - 01:41, 17 February 2010
• Category:Wave Scattering in the Marginal Ice Zone
  The marginal ice zone (MIZ) is an interfacial region that forms at the boundary of the or frozen ocean, consisting of a patchwork of ice floes and open water. Wave processes are very
  4 members (0 subcategories, 0 files) - 01:44, 17 February 2010
• The Multiple Scattering Theory of Masson and LeBlond
  for ice floes with a circular geometry. for the scattering of wave energy by ice floes.
  9 KB (1,516 words) - 01:42, 17 February 2010
• Linear Boltzmann Model for Wave Scattering in the MIZ
  ...y:Wave Scattering in the Marginal Ice Zone|Wave Scattering in the Marginal Ice Zone]]. This model effects of the individual ice floes which comprise the MIZ. To understand
  15 KB (2,588 words) - 09:30, 20 October 2009
• Dispersion Relation for a Floating Elastic Plate
  be noted that in many cases, especially for ice floes, we have infinitely deep water and can be see as a single parameter which define the ice properties. It is then very useful
  6 KB (1,064 words) - 09:36, 20 October 2009
• Main Page
  ...y:Wave Scattering in the Marginal Ice Zone|Wave Scattering in the Marginal Ice Zone]]: A description of the geophysical problem in water wave scattering.
  4 KB (559 words) - 03:27, 29 October 2012
• Three-Dimensional Floating Elastic Plate
  To determine the ice floe motion we must solve equations ((plate2)) and ( used to expand any function over the wetted surface of the ice floe <math>\Delta </math>
  9 KB (1,498 words) - 05:48, 30 October 2012
• Category:Floating Elastic Plate
  physical structures such as a floating break water, an ice floe or a [[VLFS]]). The equations of motion were formulated
  15 members (0 subcategories, 0 files) - 09:39, 20 October 2009
• Wave Forcing of Small Bodies
  developed by [[Rumer et. al. 1979]] to model the drift of ice floes in the great later used by [[Shen and Ackley 1991]] to investigate the drift of pankcake ice.
  16 KB (2,786 words) - 12:11, 11 December 2009
• Free-Surface Green Function for a Floating Elastic Plate
  We find that the spatial Fourier transform of the displacement of the ice ice sheet. This dispersion relation (and the Fourier
  17 KB (2,953 words) - 16:40, 8 December 2009
• Energy Balance for Two Elastic Plates
  The ice-covered boundary condition for the [[Floating Elastic Plate]] gives
  15 KB (2,564 words) - 09:38, 20 October 2009
• Eigenfunction Matching for a Circular Floating Elastic Plate
  the first three roots of the dispersion equation for the ice will be exactly
  17 KB (3,010 words) - 04:44, 19 July 2010
• Floating Elastic Plate on Variable Bottom Topography
  thin plate on water of constant depth was solved (to model an ice floe). One
  41 KB (6,389 words) - 09:22, 20 October 2009