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摘要: A mathematical model is reported describing the oblique reflexion and penetration of ocean waves into shore fast sea ice. The arbitrary depth allows all velocity potentials occurring in open water region to be matched precisely their counterparts ice-covered region. Matching done using a preconditioned conjugate gradient technique which complete solution found predefined precision. enables transmission coefficients at ice edge found, examples are for plates different thicknesses. critical angle predicted beyond no travelling wave penetrates sheet; this case deflexion due only evanescent modes. Critical curves provided various thicknesses on deep, intermediate shallow water. strain field set up within sheet incoming also discussed; principal strains as normal edge. Finally spreading function cover, some consequences unimodal seas with realistic functions, aim generalizing work effect an directional spectrum specified structure.