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Автор D E Weston
Дата выпуска 1961-07-01
dc.description In the sea the repeated horizontal deflection of a sound ray due to reflection at a sloping bottom produces a curvature of the horizontal path. The reflection angles in three dimensions are calculated for a sloping bottom or sound velocity interface. Even if the stratification varies in both horizontal directions there is for slow variations a simple relation between the changes in vertical and horizontal ray angle. It is then shown that the horizontal curvature may be predicted by associating a refractive index or phase velocity with each horizontal position. A formula for intensity and some illustrative problems are presented. For example it is shown that on reflection from a coastline the vertical ray angle at closest approach is equal to half the total horizontal angle through which the ray is turned.
Формат application.pdf
Издатель Institute of Physics Publishing
Название Horizontal Refraction in a Three-dimensional Medium of Variable Stratification
Тип paper
DOI 10.1088/0370-1328/78/1/308
Print ISSN 0370-1328
Журнал Proceedings of the Physical Society
Том 78
Первая страница 46
Последняя страница 52
Аффилиация D E Weston; Admiralty Research Laboratory, Teddington, Middlesex
Выпуск 1

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