Abstract
Ray theory, in spite of its approximate nature, is a very effective method for the study of sound propagation at sufficiently high frequencies in inhomogeneous media such as the ocean. In this chapter we derive the basic equations of ray acoustics and give their solutions for a stratified ocean. In later chapters the ray approach is applied to waveguide sound propagation, reflection of sound from the sea suface, and some other problems.
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References
L. M. Brekhovskikh, Yu. P. Lysanov: “Akustika okeana” (Ocean Acoustics), in Physika okeana (Ocean Physics), ed. by V. M. Kamenkovich, A. S. Monin (Nauka, Moscow 1978) Vol. 2, pp. 49–145
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H. Weinberg: J. Acoust. Soc. Am. 50, 975–984 (1971)
L. M. Brekhovskikh: Waves in Layered Media, 2nd ed. (Academic, New York 1980)
V. I. Smirnov: Kurs vyeshey matematiki 3rd ed. (GITTL, Moscow 1953) pp. 447–451 [English transl.: A Course of Higher Mathematics Vol. 4. Integral Functions and Partial Differential Equations (Pergamon, New York 1964)]
Yu. A. Kravtsov: Akust. Zh. 14, 1–24 (1968) [English transl.: Sov. Phys. Acoust. 14, 1–17 (1968)]
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© 1982 Springer-Verlag Berlin Heidelberg
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Brekhovskikh, L., Lysanov, Y. (1982). Ray Theory of the Sound Field in the Ocean. In: Fundamentals of Ocean Acoustics. Springer Series in Electrophysics, vol 8. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-02342-6_2
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DOI: https://doi.org/10.1007/978-3-662-02342-6_2
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-662-02344-0
Online ISBN: 978-3-662-02342-6
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