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1984
For centuries sea-going explorers and navigators have been aware of the dangers associated with large-amplitude surface gravity waves. Particularly frightening are the giant waves commonly found around the southern tips of South Africa and South America.
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For centuries sea-going explorers and navigators have been aware of the dangers associated with large-amplitude surface gravity waves. Particularly frightening are the giant waves commonly found around the southern tips of South Africa and South America.
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1997
Abstract : The overall goal of this PRIMER program is to assess the feasibility of the operation of a synthetic aperture sonar on the continental shelf. To evaluate the performance of this sonar system, knowledge of the fluctuations of oceanic sound speed, primarily due to internal waves, is needed.
Timothy Boyd, Murray Levine
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Abstract : The overall goal of this PRIMER program is to assess the feasibility of the operation of a synthetic aperture sonar on the continental shelf. To evaluate the performance of this sonar system, knowledge of the fluctuations of oceanic sound speed, primarily due to internal waves, is needed.
Timothy Boyd, Murray Levine
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2013
This chapter focuses on internal gravity waves in a stable thermal stratification. When the amplitude of the fluid velocity is small relative to the amplitude of the phase velocity, a linear analysis, which neglects advection, provides insight to the relation between the wavelength and frequency of internal gravity waves.
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This chapter focuses on internal gravity waves in a stable thermal stratification. When the amplitude of the fluid velocity is small relative to the amplitude of the phase velocity, a linear analysis, which neglects advection, provides insight to the relation between the wavelength and frequency of internal gravity waves.
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2003
In both the atmosphere and the ocean, the fluid is density stratified, i.e., ρ = ρ(z) (it is also a function of horizontal coordinates and time) so that usually dense fluid underlies lighter fluid. This stratification supports a new class of waves called internal waves.
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In both the atmosphere and the ocean, the fluid is density stratified, i.e., ρ = ρ(z) (it is also a function of horizontal coordinates and time) so that usually dense fluid underlies lighter fluid. This stratification supports a new class of waves called internal waves.
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2010
The study of internal gravity waves provides many challenges: they move along interfaces as well as in fully three-dimensional space, at relatively fast temporal and small spatial scales, making them difficult to observe and resolve in weather and climate models.
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The study of internal gravity waves provides many challenges: they move along interfaces as well as in fully three-dimensional space, at relatively fast temporal and small spatial scales, making them difficult to observe and resolve in weather and climate models.
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Internal gravity waves from atmospheric jets and fronts
Reviews of Geophysics, 2014Riwal Plougonven, Fuqing Zhang
exaly