Smoothed particle hydrodynamics implementation of the standard viscous–plastic sea-ice model and validation in simple idealized experiments

Abstract m s - 1) with an ellipse aspect ratio of 2, an average thickness of 1 m and free-slip boundary conditions in opposition to the FDM implementation that requires higher shear strength to simulate it. In higher-wind regimes (7.5 m s - 1) no stable ice arches are simulated – unless the thickness is increased – and the ice arch formation showed no dependence on the size of particles, in contrast to what is observed in the discrete-element framework. Finally, the SPH framework is explicit, can take full advantage of parallel processing capabilities and shows potential for pan-Arctic climate simulations.

Object Details

• Location: Deutsche Nationalbibliothek Frankfurt am Main
• Extent: Online-Ressource
• Language: Englisch

References and Relationships

• Bibliographic citation: Smoothed particle hydrodynamics implementation of the standard viscous–plastic sea-ice model and validation in simple idealized experiments ; volume:18 ; number:3 ; year:2024 ; pages:1013-1032 ; extent:20 ; The Cryosphere ; 18, Heft 3 (2024), 1013-1032 (gesamt 20)

Contributors, Places and Time

• Creator: Marquis, Oreste ; Tremblay, Bruno ; Lemieux, Jean-François ; Islam, Mohammed

Further information

• DOI: 10.5194/tc-18-1013-2024
• URN: urn:nbn:de:101:1-2024030703245939896464
• Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
• Last update: 14.08.2025, 10:44 AM CEST