Modelling wave-induced sea ice break-up in the marginal ice zone

DOI10.1098/rspa.2017.0258zbMath1404.86038arXiv1705.05941OpenAlexW3098899296WikidataQ52800785 ScholiaQ52800785MaRDI QIDQ4646861

Vernon A. Squire, Fabien Montiel

Publication date: 28 December 2018

Published in: Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences (Search for Journal in Brave)

Full work available at URL: https://arxiv.org/abs/1705.05941

zbMATH Keywords

fracturemarginal ice zonewave scatteringocean wavessea ice

Mathematics Subject Classification ID

Glaciology (86A40)

Related Items (9)

An investigation of the properties of flexural-gravity wave propagation in a coupled submerged and floating plate system ⋮ Accurate and efficient flux-corrected finite volume approximation for the fragmentation problem ⋮ Level set discrete element method for modeling sea ice floes ⋮ A two-way coupling method for simulating wave-induced breakup of ice floes based on SPH ⋮ Hydroelastic interaction between water waves and an array of circular floating porous elastic plates ⋮ Three-dimensional time-domain scattering of waves in the marginal ice zone ⋮ A fresh look at how ocean waves and sea ice interact ⋮ Study on wave-induced kinematic responses and flexures of ice floe by smoothed particle hydrodynamics ⋮ A transport equation for flexural-gravity wave propagation under a sea ice cover of variable thickness

Uses Software

• neXtSIM

Cites Work

• Attenuation and directional spreading of ocean wave spectra in the marginal ice zone
• On the calculation of an attenuation coefficient for transects of ice-covered ocean
• Past, present and impendent hydroelastic challenges in the polar and subpolar seas
• Interactions among multiple three-dimensional bodies in water waves: an exact algebraic method
• Ocean Waves
• Infinite-depth interaction theory for arbitrary floating bodies applied to wave forcing of ice floes
• Evolution of Directional Wave Spectra Through Finite Regular and Randomly Perturbed Arrays of Scatterers
• Hydroelastic response of floating elastic discs to regular waves. Part 2. Modal analysis

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