A theoretical model and an experimental model of surge motions of an ice floe due to regular waves are presented. The theoretical model is a modified version of Morrison's equation, valid for small floating bodies. The experimental model is implemented in a wave basin at a scale 1:100, using a thin plastic disc to model the floe. The processed experimental data display a regime change in surge amplitude when the incident wavelength is approximately twice the floe diameter. It is shown that the theoretical model is accurate in the high-wavelength regime, but highly inaccurate in the lowwavelength regime
Ice floes in severe Arctic seas can gain significant kinetic energy. Such a fast moving floe present...
An experimental and theoretical investigation to examine the nonlinear response of small ice masses ...
An experimental model of wave-induced collisions between two sea-ice floes is presented. The model w...
The wave-induced collisions and rafting of ice floes are investigated experimentally and theoretical...
In severe seas ice floes can gain significant kinetic energy presenting a hazard to offshore structu...
The entry of ocean waves from the open sea into pack ice is a feature of the marginal ice zone which...
An experimental model of transmission of ocean waves by an ice floe is presented. Thin plastic plate...
An experimental model is used to validate a theoretical model of a sea ice floe's flexural motion, i...
Approximately ten per cent of the ocean surface is frozen into a layer of sea ice. Ocean surface wav...
A laboratory experimental model of an incident ocean wave interacting with an ice floe is used to va...
Wind waves may play an important role in the evolution of sea ice. That role is largely determined b...
Mathematical models of ocean surface waves travelling through the sea ice covered ocean and impactin...
An attempt is made to determine whether the complex natural phenomenon of the interaction of pack ic...
Sea ice is an important indicator and agent of changes in the global climate system. The ice is affe...
Estimation of iceberg impact load is an important design consideration for offshore structures in ic...
Ice floes in severe Arctic seas can gain significant kinetic energy. Such a fast moving floe present...
An experimental and theoretical investigation to examine the nonlinear response of small ice masses ...
An experimental model of wave-induced collisions between two sea-ice floes is presented. The model w...
The wave-induced collisions and rafting of ice floes are investigated experimentally and theoretical...
In severe seas ice floes can gain significant kinetic energy presenting a hazard to offshore structu...
The entry of ocean waves from the open sea into pack ice is a feature of the marginal ice zone which...
An experimental model of transmission of ocean waves by an ice floe is presented. Thin plastic plate...
An experimental model is used to validate a theoretical model of a sea ice floe's flexural motion, i...
Approximately ten per cent of the ocean surface is frozen into a layer of sea ice. Ocean surface wav...
A laboratory experimental model of an incident ocean wave interacting with an ice floe is used to va...
Wind waves may play an important role in the evolution of sea ice. That role is largely determined b...
Mathematical models of ocean surface waves travelling through the sea ice covered ocean and impactin...
An attempt is made to determine whether the complex natural phenomenon of the interaction of pack ic...
Sea ice is an important indicator and agent of changes in the global climate system. The ice is affe...
Estimation of iceberg impact load is an important design consideration for offshore structures in ic...
Ice floes in severe Arctic seas can gain significant kinetic energy. Such a fast moving floe present...
An experimental and theoretical investigation to examine the nonlinear response of small ice masses ...
An experimental model of wave-induced collisions between two sea-ice floes is presented. The model w...