Viscous–Plastic Sea Ice Dynamics with the EVP Model: Linearization Issues

By Elizabeth C. Hunke. 2001

248 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/88ab00217e95a757869e1873698840fd07c039f5

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In Atmospheric Science

Citations in the corpus

On the formulation of sea-ice models. Part 1: Effects of different solver implementations and parameterizations (2010, methodology): “The differences between LSOR and EVP can, in571 part, stem from incomplete convergence of the solvers due to linearization and572 due to different methods of linearization (Hunke, 2001, and B. Tremblay, pers.573 comm. 2008).”
Ridging, strength, and stability in high-resolution sea ice models (2007, background): “Hunke, W. Maslowski, and J. Jakacki (2007), Ridging, strength, and stability in high-resolution sea”
Ocean forecasting in terrain-following coordinates: Formulation and skill assessment of the Regional Ocean Modeling System (2008, unknown): “(2007), doi:10.1016/j.jcp.2007.06.016 Plea put. o H zuð Þ ot þ o uH zuð Þ ox þ o vH zuð Þ oy þ o XHzuð Þ os fH zv ¼ H z q0 op ox Hzg of ox o os u0w0 m H z ou os ; ð1Þ o H zvð Þ ot þ o uH zvð Þ ox þ o vH zvð Þ oy þ o XHzvð Þ os þ fH zu ¼ H z q0 op oy Hzg of oy o os v0w0 m H z ov os ; ð2Þ 0 ¼ 1 q0 op…”
The Elastic Viscous Plastic Sea Ice Dynamics Model in General Orthogonal Curvilinear Coordinates on a Sphere—Incorporation of Metric Terms (2002, methodology): “The second formulation features other desirable properties, including a new definition of the elastic parameter E that allows elastic waves to damp out more quickly and ensures that the internal stresses converge to the elliptical yield surface appropriately (Hunke 2001).”
Finite-Element Sea Ice Model (FESIM), version 2 (2015, methodology): “It can be circumvented by limiting “viscosities” (ζ = P0/2(1+1min),η = ζ/e 2) so that they stay below some level (see Hunke, 2001) P0/((1+1min) ClimT1x 2/(1tEVP) 2, whereClim is the limiting constant and 1x the grid cell size.”