An idealized wave-ice interaction model without subgrid spatial or temporal discretizations
A new numerical implementation is proposed for a wave–ice interaction model. It is applied to an idealized transect geometry. Wave attenuation due to ice floes and wave-induced ice fracture are both included in the model. The new method alleviates the need for subgrid spatial or temporal discretizat...
Published in: | Annals of Glaciology |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
International Glaciological Society
2015
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Subjects: | |
Online Access: | http://hdl.handle.net/2440/95708 https://doi.org/10.3189/2015AoG69A599 |