An unstructured C-grid type variational formulation for the sea ice dynamics
Historically, B-grid formulations of sea ice dynamics have been dominant because they have matched the grid type used by ocean models. The reason for the grid match is simple - it facilitates penetration of the curl of ice-ocean stress into the deep ocean with minimal numerical diffusivity because s...
Main Authors: | , , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
arXiv
2021
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Subjects: | |
Online Access: | https://dx.doi.org/10.48550/arxiv.2112.14993 https://arxiv.org/abs/2112.14993 |