Mathematical models of ocean surface waves travelling through the sea ice covered ocean and impacting the ice cover have been developed for over 40 years now. The kernel of the models is a model of water waves interacting with a solitary ice floe. The ice floe is conventionally modelled as thin floating elastic plate. Water motions are conventionally modelled using potential flow theory
An attempt is made to determine whether the complex natural phenomenon of the interaction of pack ic...
Published online 24 August 2011Exponential attenuation of ocean surface waves in ice-covered regions...
A laboratory experimental model of an incident ocean wave interacting with an ice floe is used to va...
The entry of ocean waves from the open sea into pack ice is a feature of the marginal ice zone which...
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...
Sea ice is an important indicator and agent of changes in the global climate system. The ice is affe...
An experimental model of transmission of ocean waves by an ice floe is presented. Thin plastic plate...
A model of the extent of wave driven overwash into fields of sea ice floes is proposed. The extent m...
A wave-ice interaction model for the marginal ice zone (MIZ) is reported that calculates the attenua...
The outer edge of the sea ice cover, also known as marginal ice zone (MIZ), is the area where the in...
Global warming is inducing sea ice retreat, which is opening new shipping routes and extending the a...
A theoretical model of water wave overwash of a thin floating plate is proposed. The nonlinear shall...
· Experimental validation of a mathematical model of wave-induced flexural motion of a thin floating...
Two- and three-dimensional models are proposed for ocean-wave attenuation due to scattering by ice f...
An attempt is made to determine whether the complex natural phenomenon of the interaction of pack ic...
Published online 24 August 2011Exponential attenuation of ocean surface waves in ice-covered regions...
A laboratory experimental model of an incident ocean wave interacting with an ice floe is used to va...
The entry of ocean waves from the open sea into pack ice is a feature of the marginal ice zone which...
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...
Sea ice is an important indicator and agent of changes in the global climate system. The ice is affe...
An experimental model of transmission of ocean waves by an ice floe is presented. Thin plastic plate...
A model of the extent of wave driven overwash into fields of sea ice floes is proposed. The extent m...
A wave-ice interaction model for the marginal ice zone (MIZ) is reported that calculates the attenua...
The outer edge of the sea ice cover, also known as marginal ice zone (MIZ), is the area where the in...
Global warming is inducing sea ice retreat, which is opening new shipping routes and extending the a...
A theoretical model of water wave overwash of a thin floating plate is proposed. The nonlinear shall...
· Experimental validation of a mathematical model of wave-induced flexural motion of a thin floating...
Two- and three-dimensional models are proposed for ocean-wave attenuation due to scattering by ice f...
An attempt is made to determine whether the complex natural phenomenon of the interaction of pack ic...
Published online 24 August 2011Exponential attenuation of ocean surface waves in ice-covered regions...
A laboratory experimental model of an incident ocean wave interacting with an ice floe is used to va...