Titlebook: Computational Ocean Acoustics; Finn B. Jensen,William A. Kuperman,Henrik Schmidt Textbook 2011Latest edition Springer Science+Business Med

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書目名稱Computational Ocean Acoustics影響因子(影響力)




書目名稱Computational Ocean Acoustics影響因子(影響力)學(xué)科排名




書目名稱Computational Ocean Acoustics網(wǎng)絡(luò)公開度




書目名稱Computational Ocean Acoustics網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Computational Ocean Acoustics被引頻次




書目名稱Computational Ocean Acoustics被引頻次學(xué)科排名




書目名稱Computational Ocean Acoustics年度引用




書目名稱Computational Ocean Acoustics年度引用學(xué)科排名




書目名稱Computational Ocean Acoustics讀者反饋




書目名稱Computational Ocean Acoustics讀者反饋學(xué)科排名

Ancestor

不可思議

Ray Methods,or ray tracing and primarily the latter. Today, however, ray tracing codes have fallen somewhat out of favor in the research community, the problem being the inherent (high frequency) approximation of the method which leads to somewhat coarse accuracy in the results. On the other hand, ray methods a

Silent-Ischemia

insurgent

Normal Modes,e theory for a simple two-layer model of the ocean. At about the same time Ide?et al.?[2] had been using normal modes to interpret propagation in the Potomac River and Chesapeake Bay. Progress in the development of normal-mode methods is presented in an excellent summary given by Williams?[3]. Numer

書法

Parabolic Equations,ve propagation in the atmosphere. Since then, parabolic equations have been used in several branches of physics, including the fields of optics, plasma physics, seismics, and underwater acoustics. It is the application of PE methods to wave-propagation problems in the ocean that is the subject of th

書法

Finite Differences and Finite Elements,re of these approaches are numerically efficient for the majority of forward problems occurring in underwater acoustics, including propagation over very long ranges, with or without lateral variations in the environment. However, the numerical efficiency of these approaches is obtained by sacrificin

Enzyme

Broadband Modeling,Earth’s crust, underwater acousticians have traditionally favored spectral analysis techniques, which only provide information about the band-averaged energy distribution in space. There are several reasons for choosing this approach in ocean acoustics. Most importantly, the ocean is characterized b

boisterous

Ambient Noise,ise in the ocean impacts underwater acoustics in two ways: It is the resident acoustic field in the ocean and hence also a diagnostic of the ocean environment. It is the interference with respect to detecting or measuring signals.

決定性