Titlebook: High-Frequency Seafloor Acoustics; Darrell R. Jackson,Michael D. Richardson Book 2007 Springer-Verlag New York 2007 Geophysics.High-freque

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Brittle

縮影

Fluid Theories,t can account for the phenomena evident in the data at hand. Because of the close relationships between the various theories, the discussion of research issues will be unified and placed at the end of Ch. 10.

LIEN

GNAW

Book 2007s of the seas. For over sixty years The United States Office of Naval Research (ONR) has been a major sponsor of undersea research and development at universities, national laboratories, and industrial organizations. App- priately ONR is the sponsor of this monograph series. The intent of the series

中和

蔓藤圖飾

詳細(xì)目錄

Roughness Scattering Models,s is the type of microtopography discussed in Ch. 6. This work is the primary subject of this chapter, but recent work on scattering due to discrete roughness features, such as shell fragments lying on the sediment-water interface, will be treated briefly.

Androgen

Introduction, the seafloor is a source of interfering reverberation that degrades the desired target echo signal. On the other hand, when sonar is used to observe or characterize the seafloor, scattering provides the desired signal. In either case, an understanding of scattering by the seafloor can provide benefits in sonar design and application.

SAGE

Sediment Heterogeneity, this heterogeneity and is dependent on its magnitude and spatial scale. The effects of physical, biological, and biogeochemical processes on the internal 3D structure of sediments and the spatial distribution of values of sediment physical properties were reviewed in Ch. 3.