Titlebook: Ocean Acoustics; John A. DeSanto Book 1979 Springer-Verlag Berlin Heidelberg 1979 Meer.Ocean.Schallausbreitung.Wasserschall.acoustics.hydr

parsimony

Introduction,d, and the relationship can be expressed mathematically. The second and more recent aspect is concerned with the use of acoustics as a tool to prove the oceanic structure. For example, acoustics can be used to monitor ocean currents in the sense that characteristic modifications of the acoustic field infer local changes in the ocean current.

Connotation

Oceanography in Underwater Acoustics,ention. Next, the subjects of internal waves and fine structure representing horizontal scales of tens of meters to order ten kilometers are presented. Finally, we include a short discussion of the scales of variability in the near-surface mixed layer.

減震

Theoretical Methods in Ocean Acoustics,first describe the properties of the fluid equations. We derive equations for these properties in Sect.2.1 from first principles, but briefly, and then obtain the equations governing the sound field which we discuss in more detail in the remaining parts of this chapter.

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認識

Ocean Acoustics978-3-642-81294-1Series ISSN 0342-6793

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侵害

https://doi.org/10.1007/978-3-642-81294-1Meer; Ocean; Schallausbreitung; Wasserschall; acoustics; hydrogeology