Titlebook: Ocean Seismo-Acoustics; Low-Frequency Underw Tuncay Akal,Jonathan M. Berkson Book 1986 Springer Science+Business Media New York 1986 Arctic

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J. Miller,A. Nagl,H. überallelbarer Erw?rmung wird die W?rmeenergie von au?en an das Schmelzgut herangebracht und geht durch W?rmeleitung, Konvektion, W?rmestrahlung oder elektromagnetische Strahlung auf das Gut über. Die unmittelbare Erw?rmung dagegen l??t die W?rme im Gut selbst entstehen. Auch Grenzf?lle zwischen unmittelba

Accede

chronicle

Homer P. Bucker,Michael B. Porterelbarer Erw?rmung wird die W?rmeenergie von au?en an das Schmelzgut herangebracht und geht durch W?rmeleitung, Konvektion, W?rmestrahlung oder elektromagnetische Strahlung auf das Gut über. Die unmittelbare Erw?rmung dagegen l??t die W?rme im Gut selbst entstehen. Auch Grenzf?lle zwischen unmittelba

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MIR

Bottom Interaction Effects on Normal Modes: an Algebraic Approach

鉆孔

有花

Intrinsic Modes in a Wedge-Shaped Ocean with Stratified Elastic Bottomlanted interface. The model is now generalized to allow for stratification of the slanted bottom along planes parallel to the water-bottom interface, and for elastic properties in these layers. Examined in detail is the special case where the bottom is an elastic half space. Upslope propagation in t

LEVER

An Acoustic Reflectivity Method for Laterally Varying Layered Mediabed as a stack of plane parallel layers; however, within each layer the velocity, density, and quality factor, Q, are now functions of horizontal position x. These functions are all independent from layer to layer so any earth or sea-bed model can be parameterized in this way. The two foundations of

Lumbar-Spine

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Gaussian Beams and 3-D Bottom Interacting Acoustic Systemsy differential equation along the central ray. This latter method has recently received a lot of attention in the seismological community. Both methods are free of the difficulties at caustics and in shadow zones which afflict standard ray tracing algorithms. Comparisons are presented between the st