Results 211 to 220 of about 129,873 (262)
An Improved Method for Measuring Acoustic Attenuation in Viscoelastic Solid Media. [PDF]
Fa L +8 more
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Deep learning-based oceanic internal wave detection from SWOT satellite imaginary observations. [PDF]
Pang S, Su X, Yang S.
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Data Quality Assessment, Representativeness, and External Consistency of a Coastal Oceanographic Buoy Using Copernicus Marine and ERA5 Products. [PDF]
Portillo F +6 more
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Design strategies of polyvinyl alcohol-based composites for EMI shielding: from matrix modulation to structural engineering. [PDF]
Zheng R, Yang J, Weng Z, Xiong Y.
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A 46-Year-Old Man Presenting With Chest Pain Due to Apical Hypertrophic Cardiomyopathy (Yamaguchi Syndrome) Diagnosed by Multimodal Cardiac Imaging. [PDF]
Passos MD +5 more
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Proceedings of the European Wave and Tidal Energy Conference, 2023
Internal waves are ubiquitous oceanographic features that occur in various forms across the world’s oceans. They manifest themselves as interface waves across ocean density layers that represent the interplay between buoyancy and gravitational forces, and are typically classified as linear and nonlinear internal waves.
Kaustubha Raghukumar +3 more
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Internal waves are ubiquitous oceanographic features that occur in various forms across the world’s oceans. They manifest themselves as interface waves across ocean density layers that represent the interplay between buoyancy and gravitational forces, and are typically classified as linear and nonlinear internal waves.
Kaustubha Raghukumar +3 more
openaire +1 more source
Studies in Applied Mathematics, 1992
The expansion procedure introduced by Benney (1966) for weakly nonlinear, planar shallow‐water waves is used to provide an alternative derivation of the more general results of Benjamin (1966) for shallow fluid layers possessing arbitrary vertical stratification and horizontal shear.
Weidman, P. D., Velarde, M. G.
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The expansion procedure introduced by Benney (1966) for weakly nonlinear, planar shallow‐water waves is used to provide an alternative derivation of the more general results of Benjamin (1966) for shallow fluid layers possessing arbitrary vertical stratification and horizontal shear.
Weidman, P. D., Velarde, M. G.
openaire +1 more source

