Titlebook: Bottom-Interacting Ocean Acoustics; William A. Kuperman,Finn B. Jensen Book 1980 Springer Science+Business Media New York 1980 Ocean.acous

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书目名称Bottom-Interacting Ocean Acoustics影响因子(影响力)




书目名称Bottom-Interacting Ocean Acoustics影响因子(影响力)学科排名




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书目名称Bottom-Interacting Ocean Acoustics网络公开度学科排名




书目名称Bottom-Interacting Ocean Acoustics被引频次




书目名称Bottom-Interacting Ocean Acoustics被引频次学科排名




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书目名称Bottom-Interacting Ocean Acoustics读者反馈学科排名

monologue

敌手

Alexander A. Prokopenko,Douglas F. Williamsment of the fluid relative to the solid frame. Both losses can be included in the Biot theory for sound propagation in porous media. This theory gives an attenuation coefficient for the frictional loss that is proportional to the frequency, f, and, a viscous attenuation increasing as f. at low frequ

Intercept

Alexander A. Prokopenko,Douglas F. Williamsr. Knowledge of these properties enables one to derive the complex reflection factor under arbitrary angles of incidence, which is an important quantity in modelling sound propagation. Though preference has been given to all methods that operate remotely, no successful breakthrough has yet been achi

水獭

殖民地

bacteria

Alexander A. Prokopenko,Douglas F. Williamsown to a depth of about 70 m below the sediment surface. Several different structures due to high gas contents are described and explained for the first time in the northern Adriatic. They range from the so-called “basin effect” and cone-like structures to acoustic voids. Gas seeping from the bottom

THROB

Characteristics of World Leadershipities from the echosounder returns, sidescan sonar and sub-bottom profiling, supplemented by surface samples and cores, are compared. The reflection intensities are integrated from the echoes of the top 75 cm of sediment. The instrument is very sensitive to slight changes in the composition of muds

诱骗

Characteristics of World Leadershiptions from the Southeast Asian shelves and marginal basins. The velocity functions are least-squares regressions of the form V = V. + Kt, where t is one-way vertical travel-time to layer mid-points. The value of K shows surprisingly little variability on the shelves and adjoining basins from the Bay

异教徒

Characteristics of World Leadershippic. Physical models have been developed and refined which can both explain the observations and serve as a basis for predictions. Examples will be presented which contrast values determined from the physical models with measured data in order to identify problem areas and to recommend directions fo