<abstract xmlns="http://www.w3.org/1999/xhtml"><p> The paper is concerned with the problem of sea-ice pack motion and deformation under the action of wind and water currents. Differential equations describing the dynamics of ice, with its very distinct mateFfigrial responses in converging and diverging flows, express the mass and linear momentum balances on the horizontal plane (the free surface of the ocean). These equations are solved by the fully Lagrangian method of smoothed particle hydrodynamics (SPH). Assuming that the ice behaviour can be approximated by a non-linearly viscous rheology, the proposed SPH model has been used to simulate the evolution of a sea-ice pack driven by wind drag stresses. The results of numerical simulations illustrate the evolution of an ice pack, including variations in ice thickness and ice area fraction in space and time. The effects of different initial ice pack configurations and of different conditions assumed at the coast-ice interface are examined. In particular, the SPH model is applied to a pack flow driven by a vortex wind to demonstrate how well the Lagrangian formulation can capture large deformations and displacements of sea ice.</p></abstract>

The paper is concerned with the problem of sea-ice pack motion and deformation under the action of wind and water currents. Differential equations describing the dynamics of ice, with its very distinct mateFfigrial responses in converging and diverging flows, express the mass and linear momentum balances on the horizontal plane (the free surface of the ocean). These equations are solved by the fully Lagrangian method of smoothed particle hydrodynamics (SPH). Assuming that the ice behaviour can be approximated by a non-linearly viscous rheology, the proposed SPH model has been used to simulate the evolution of a sea-ice pack driven by wind drag stresses. The results of numerical simulations illustrate the evolution of an ice pack, including variations in ice thickness and ice area fraction in space and time. The effects of different initial ice pack configurations and of different conditions assumed at the coast-ice interface are examined. In particular, the SPH model is applied to a pack flow driven by a vortex wind to demonstrate how well the Lagrangian formulation can capture large deformations and displacements of sea ice.

SPH Modelling of Sea-ice Pack Dynamics

Archives of Hydro-Engineering and Environmental Mechanics

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

{"article-title":"SPH Modelling of Sea-ice Pack Dynamics"}

The paper is concerned with the problem of sea-ice pack motion and deformation under the action of wind and water currents. Differential equations describing...

SPH Modelling of Sea-ice Pack Dynamics

Publicado en línea: 23 ene 2018

Páginas: 115 - 137

Recibido: 19 nov 2017

Aceptado: 27 dic 2017

DOI: https://doi.org/10.1515/heem-2017-0008

Palabras clave
sea-ice dynamics, Lagrangian description, smoothed particle hydrodynamics, moving boundary problem

© by Ryszard Staroszczyk

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

SPH Modelling of Sea-ice Pack Dynamics

Publicado en línea: 23 ene 2018

Páginas: 115 - 137

Recibido: 19 nov 2017

Aceptado: 27 dic 2017

DOI: https://doi.org/10.1515/heem-2017-0008

Palabras clavesea-ice dynamics, Lagrangian description, smoothed particle hydrodynamics, moving boundary problem

© by Ryszard Staroszczyk

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

Palabras clave
sea-ice dynamics, Lagrangian description, smoothed particle hydrodynamics, moving boundary problem