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Titlebook: Ocean Variability & Acoustic Propagation; John Potter,Alex Warn-Varnas Book 1991 Springer Science+Business Media Dordrecht 1991 Ocean

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书目名称Ocean Variability & Acoustic Propagation
编辑John Potter,Alex Warn-Varnas
视频video
图书封面Titlebook: Ocean Variability & Acoustic Propagation;  John Potter,Alex Warn-Varnas Book 1991 Springer Science+Business Media Dordrecht 1991 Ocean
描述Fifteen years ago NATO organised a conference entitled ‘Ocean Acoustic Modelling‘. Many of its participants were again present at this variability workshop. One such participant. in concluding his 1975 paper, quoted the following from a 1972 literature survey: ‘ ... history presents a sad lack of communications between acousticians and oceanographers‘ Have we done any better in the last 15 years? We believe so, but only moderately. There is still a massive underdeveloped potential for acousticians and oceanographers to make significant progress together. Currently, the two camps talk together insufficiently even to avoid simple misun­ derstandings. such as those in Table 1. Table 1 Ocsanographic and acoustic jargon (from an idea by Pol/ardi Jargon Oceanographic use Acoustic use dbordB decibar (depth in m) decibel (energy level) PE primitive equations parabolic equations convergence zone converging currents converging rays (downwelling water) (high energy density) front thermohaline front wave, ray or time front speed water current speed sound propagation speed 1 The list goes on.
出版日期Book 1991
关键词Ocean
版次1
doihttps://doi.org/10.1007/978-94-011-3312-8
isbn_softcover978-94-010-5462-1
isbn_ebook978-94-011-3312-8
copyrightSpringer Science+Business Media Dordrecht 1991
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The Effects of Sound Speed on the Shape of the Ocean Impulse Responsee sound speed cases. It is found that the envelopes of these responses are predictable enough to remove propagational distortion by deconvolving the data envelope with the model envelope and thus extract useful source signal characteristics.
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Summary of Session 1ic scintillation and tomography inverses). Appropriate partitions between deterministic processes (e.g. tides and fronts) and stochastic processes was an important theme. This theme and many others continued through the week, hence, it is not useful to summarize the discussions held only on Monday.
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Two Dimensional Acoustical Propagation in a Stratified Shear Flowzontal over scales of <10m. The two-dimensional angle of arrival distribution is correlated during strongly sheared flow, a result that can be explained in terms of the passage of inclined planes of higher density fluid associated with shear flow instabilities passing through the acoustical path.
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Nonlinear Effects in Wind-Wave Generation, cross-spectra of signals from gauge-pairs were computed to investigate the statistical relationship between frequency and wavenumber. The results are modeled by a method similar to that used in the analysis of turbulent flow.
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