Abstract
In this chapter, we will consider some simple models of the shallow water waveguide. Such models allow us to obtain and understand the main features of SW sound propagation quickly. Such simple models can also be perturbed to take into account more realistic properties of the environment, thus giving them far more power than one might think at first.
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Notes
- 1.
The dependence of density on the spatial coordinates can be easily taken into account using a change of functions (see Sect. 3.3). The possibility of some depth dependence of the bottom properties is also discussed.
- 2.
This field is the Green function of the waveguide, determined by the general equation (A.162); in what follows, when not required in the problem, we shall omit the arguments \( {\vec{R}_0},\,\omega \).
- 3.
The function \( g(\xi ) \) is related to the impedance of the bottom\( {Z_1} \) by the equation \( g(\xi ) = i{Z_1}{/}\omega \rho \), where the impedance is defined according to Brekhovskikh (1980); the change in sign from Brekhovskikh (1980) is due to the direction of the z-axis. It also is related to the bottom reflection coefficient by \( V = {{{( {g\sqrt {{{k^2}(H) - {\xi^2}}} + i})}} / {{({g\sqrt {{{k^2}(H) - {\xi^2}}} - i})}}.} \)
- 4.
In other sections we shall neglect the contribution of the continuous spectrum, and the notation \( \Psi \) will be used for the field generated by the discrete spectrum.
- 5.
Strictly speaking we should write for every vertical mode \( {x_l}(y) \) and \( {y_l}(x) \). However, for simplicity we will omit subscript.
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Katsnelson, B., Petnikov, V., Lynch, J. (2012). Foundations of the Theory of Propagation of Sound. In: Fundamentals of Shallow Water Acoustics. The Underwater Acoustics Series. Springer, Boston, MA. https://doi.org/10.1007/978-1-4419-9777-7_3
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