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Titlebook: Ocean Acoustics; John A. DeSanto Book 1979 Springer-Verlag Berlin Heidelberg 1979 Meer.Ocean.Schallausbreitung.Wasserschall.acoustics.hydr

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发表于 2025-3-21 19:23:10 | 显示全部楼层 |阅读模式
书目名称Ocean Acoustics
编辑John A. DeSanto
视频video
丛书名称Topics in Current Physics
图书封面Titlebook: Ocean Acoustics;  John A. DeSanto Book 1979 Springer-Verlag Berlin Heidelberg 1979 Meer.Ocean.Schallausbreitung.Wasserschall.acoustics.hydr
描述This Topics volume is devoted to a study of sound propagation in the ocean. The effect of the interior of the ocean on underwater sound is analogous to the effect of a lens on light. The oceanic lens is related, as in light propagation, to the index of refraction of the medium. The latter is giv~n by the ratio of the sound frequency to the speed of sound in water, typi ca lly about 1500 m s -1. It is the vari­ ation of the sound speed due to changing temperature, density, salinity, and pres­ sure in the complex ocean environment which creates the lens effect. Many oceanic processes such as currents, tides, eddies (circulating, translating regions of wa­ ter), and internal waves (the wave-like structure of the oceanic density variabil­ ity) contri bute in turn to the changes in sound speed‘. The net effect of the ocean lens is to trap and guide sound waves in a channel created by the lens. The trapped sound can then propagate thousands of miles in this oceanic waveguide. In addition to the propagation in the interior of the ocean, sound can propagate into and back out of the ocean bottom as well as scatter from the ocean surface. Just as the sound produced by a loudspeaker in a room
出版日期Book 1979
关键词Meer; Ocean; Schallausbreitung; Wasserschall; acoustics; hydrogeology
版次1
doihttps://doi.org/10.1007/978-3-642-81294-1
isbn_softcover978-3-642-81296-5
isbn_ebook978-3-642-81294-1Series ISSN 0342-6793
issn_series 0342-6793
copyrightSpringer-Verlag Berlin Heidelberg 1979
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书目名称Ocean Acoustics影响因子(影响力)




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Numerical Models of Underwater Acoustic Propagation,n automated computer code capable of being executed by someone other than the originator for a wide variety of problems. No single model currently exists which is adequate for all applications. This is perhaps not surprising considering the diversity of the ocean environment and its boundaries, and
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Physical Modeling of Underwater Acoustics,veloped. These include, but are not limited to, mathematical analysis, numerical modeling, in situ empirical description, and physical modeling. All have made substantial contributions to our understanding of the way in which sound behaves in water. The purpose of this chapter is to review the metho
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Oceanography in Underwater Acoustics,ctions, after a discussion of the important physical parameters, follows the scales of variations that exist in the ocean. First, the oceanic “climate” that is represented by mean ocean basin scale conditions with its seasonal changes is presented. Then, the ocean “weather” that is represented by ed
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Acoustic Probing of Space-Time Scales in the Ocean,derate our weather. The Gulf Stream changes shape and location in rough approximation to the seasons. The weather on the East Coast of the United States may worsen significantly if the stream moves further offshore. These circulating waters also carry nutrients essential to the maintenance of fishin
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Numerical Models of Underwater Acoustic Propagation, of the wave equation found in Sect.2.2.1. Fundamentally these models consider the ocean to be a deterministic environment for which the speed of sound is only a function of the spatial coordinates. Non-deterministic effects, if accounted for at all, are included in an ad hoc fashion following the d
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Physical Modeling of Underwater Acoustics,anks and particularly with the study of surface scattering in such facilities. Physical model research has been conducted for some time in a number of contexts. Unfortunately, until the present there has been little communication among various investigators on matters of technique. By discussing the
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