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

誤解

書目名稱Bottom-Interacting Ocean Acoustics影響因子(影響力)




書目名稱Bottom-Interacting Ocean Acoustics影響因子(影響力)學科排名




書目名稱Bottom-Interacting Ocean Acoustics網(wǎng)絡(luò)公開度




書目名稱Bottom-Interacting Ocean Acoustics網(wǎng)絡(luò)公開度學科排名




書目名稱Bottom-Interacting Ocean Acoustics被引頻次




書目名稱Bottom-Interacting Ocean Acoustics被引頻次學科排名




書目名稱Bottom-Interacting Ocean Acoustics年度引用




書目名稱Bottom-Interacting Ocean Acoustics年度引用學科排名




書目名稱Bottom-Interacting Ocean Acoustics讀者反饋




書目名稱Bottom-Interacting Ocean Acoustics讀者反饋學科排名

monologue

敵手

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

水獺

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

誘騙

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

異教徒

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