INFER 发表于 2025-3-21 19:42:46
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Weakly Nonlinear Water Waves Propagating over Uneven Bottoms,ffects of ambient currents. These extensions result in a couple of equations, i.e. a general third-order evolution equation for the envelope of a modulated wave train with a current over an uneven bottom and an equation of the second-order (locked and free) long waves induced by the modulated wave train.减少 发表于 2025-3-22 00:50:59
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current interactions over arbitrary depth.Covers an extended.Wave motion is one of the broadest scientific subjects in nature, especially water waves in the near-shore region which present more richness and complexity of variability with respect to deep-water waves. .Dynamics of Surface Waves in CoaSputum 发表于 2025-3-22 14:20:13
Specimen Examination Paper Number 2,two ones for wave-current interactions concerning both a two-layer approach with an infinitely deep fluid and an .-layer approach with the lowest fluid over uneven bottoms, and one consisting of an .-layer of pure waves.Sputum 发表于 2025-3-22 17:36:48
Book 2009Latest editionplexity of variability with respect to deep-water waves. .Dynamics of Surface Waves in Coastal Waters: Wave-Current-Bottom Interactions. develops the typical basic theories (e.g. mild-slope equation and shore-crested waves) and applications of water wave propagation with an emphasis on wave-current-印第安人 发表于 2025-3-22 22:29:09
https://doi.org/10.1007/978-1-349-09277-2maller than that of the water depth. Including the effect of evanescent modes, the second depends on a generally varying bottom without prescribed assumption, and covers a number of special and typical mild-slope equations with and without porous layers.adequate-intake 发表于 2025-3-23 03:37:10
Linear Gravity Waves over Rigid, Porous Bottoms,maller than that of the water depth. Including the effect of evanescent modes, the second depends on a generally varying bottom without prescribed assumption, and covers a number of special and typical mild-slope equations with and without porous layers.小故事 发表于 2025-3-23 08:33:42
Hamiltonian Description of Stratified Wave-Current Interactions,two ones for wave-current interactions concerning both a two-layer approach with an infinitely deep fluid and an .-layer approach with the lowest fluid over uneven bottoms, and one consisting of an .-layer of pure waves.