期刊
OCEAN MODELLING
卷 27, 期 3-4, 页码 174-184出版社
ELSEVIER SCI LTD
DOI: 10.1016/j.ocemod.2009.01.004
关键词
Sea ice; Coupled sea ice-ocean model; Elastic-viscous-plastic rheology; Model grid
资金
- United Kingdom's Natural Environment Research Council
- Belgian Federal Science Policy Office
- NERC [pol010005] Funding Source: UKRI
- Natural Environment Research Council [pol010005] Funding Source: researchfish
The elastic-viscous-plastic (EVP) sea ice rheology has been introduced in the large-scale Louvain-la-Neuve sea-Ice Model, version 2 (LIM2), and its performance has been evaluated. Centred difference versions of the rheology have been implemented on both an Arakawa B grid and a C grid, and their performance have been intercompared in coupled simulations with the Nucleus for European Modelling of the Ocean (NEMO) model. Integrations with both implementations lead to fairly similar results which compare well with observations and with previous LIM simulations. The C grid version, however, offers a number of advantages: (a) easier ice coupling with NEMO, which is itself defined on a C grid; (b) possibility of representing ice transport across one-cell-wide straits and passages; (c) better representation of inertial-plastic compressive waves. For these reasons, we recommend the use of the C grid EVP formulation of the ice dynamics in future LIM applications. (C) 2009 Elsevier Ltd. All rights reserved.
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