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Titlebook: Ocean Seismo-Acoustics; Low-Frequency Underw Tuncay Akal,Jonathan M. Berkson Book 1986 Springer Science+Business Media New York 1986 Arctic

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书目名称Ocean Seismo-Acoustics
副标题Low-Frequency Underw
编辑Tuncay Akal,Jonathan M. Berkson
视频video
丛书名称Nato Conference Series
图书封面Titlebook: Ocean Seismo-Acoustics; Low-Frequency Underw Tuncay Akal,Jonathan M. Berkson Book 1986 Springer Science+Business Media New York 1986 Arctic
描述Seafloor investigation has long been a feature of not only seismology but also of acoustics. Indeed it was acoustics that produced depth sounders, giving us the first capability of producing both global and local maps of the seafloor. Subsequently, better instrumentation and techniques led to a clearer, more quantitative picture of the seabed itself, which stimulated new hypotheses such as seafloor spreading through the availability of more reliable data on sediment thickness over ocean basins and other bottom features. Geologists and geophysicists have used both acoustic and seismic methods to study the seabed by considering the propagation of signals arising from both natural seismic events and man-made impulsive sources. Although significant advances have been made in instrumentation, such as long towed geophysical arrays, ai r guns and ocean bot tom seismometers, the pic ture of the seafloor is still far from complete. Underwater acoustics concerns itself today with the phenomena of propagation and noise at frequencies and ranges that require an understanding of acoustic interaction at both of its boundaries, the sea surface and seafloor, over depths ranging from tens to thousa
出版日期Book 1986
关键词Arctic Ocean; Coast; Helmholtz equation; acoustics; marine; noise; ocean; scattering; seismology
版次1
doihttps://doi.org/10.1007/978-1-4613-2201-6
isbn_softcover978-1-4612-9293-7
isbn_ebook978-1-4613-2201-6
copyrightSpringer Science+Business Media New York 1986
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Development of a Parabolic Approximation for the Computation of Propagation Loss in a Range-Dependenolution for a quadratic development of the propagation operator which allows us to take into account a larger angular aperture of the source. The numerical solution is given by an algorithm of finite differences using the Crank-Nicholson method. The problem of rectilinear, horizontal and oblique int
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Linear and Nonlinear Ocean Acoustic Propagation Modelsfluid dynamics a nonlinear time domain wave equation is then derived. A unidirectional approximation leads to a nonlinear time domain version of the parabolic equation, a nonlinear progressive wave equation (NPE), which can treat propagation of finite amplitude signals in a refracting medium in a wa
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