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The ampli tude a nd phase of th e groundwave are calculated fo r oblique propagaLion across a flat lyin g coas tline. The land a nd sea are assumed to be smooth a nd homo"eneous. Atten tion is focll sed on the effects which t ak e place neal' t he coastlin e. It. is shown t hat the reflected wave d ep ends c ri ticall y on the a ngle of incidence, 00 , while the tran smi tted wave has only a weak d ependence on 0".
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James R. Wait (1963) studied this question.
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