標(biāo)題: Titlebook: Dynamics of Surface Waves in Coastal Waters; Wave-Current-Bottom Hu Huang Book 2009Latest edition Springer-Verlag Berlin Heidelberg 2009 H [打印本頁(yè)] 作者: INFER 時(shí)間: 2025-3-21 19:42
書(shū)目名稱Dynamics of Surface Waves in Coastal Waters影響因子(影響力)
書(shū)目名稱Dynamics of Surface Waves in Coastal Waters影響因子(影響力)學(xué)科排名
書(shū)目名稱Dynamics of Surface Waves in Coastal Waters網(wǎng)絡(luò)公開(kāi)度
書(shū)目名稱Dynamics of Surface Waves in Coastal Waters網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書(shū)目名稱Dynamics of Surface Waves in Coastal Waters被引頻次
書(shū)目名稱Dynamics of Surface Waves in Coastal Waters被引頻次學(xué)科排名
書(shū)目名稱Dynamics of Surface Waves in Coastal Waters年度引用
書(shū)目名稱Dynamics of Surface Waves in Coastal Waters年度引用學(xué)科排名
書(shū)目名稱Dynamics of Surface Waves in Coastal Waters讀者反饋
書(shū)目名稱Dynamics of Surface Waves in Coastal Waters讀者反饋學(xué)科排名
作者: Admonish 時(shí)間: 2025-3-21 21:41
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.作者: 減少 時(shí)間: 2025-3-22 00:50 作者: 藝術(shù) 時(shí)間: 2025-3-22 06:48 作者: Mucosa 時(shí)間: 2025-3-22 11:30
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 Coa作者: Sputum 時(shí)間: 2025-3-22 14:20
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.作者: Sputum 時(shí)間: 2025-3-22 17:36
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-作者: 印第安人 時(shí)間: 2025-3-22 22:29
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.作者: adequate-intake 時(shí)間: 2025-3-23 03:37
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.作者: 小故事 時(shí)間: 2025-3-23 08:33
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.作者: HALO 時(shí)間: 2025-3-23 11:07
Equal Opportunities in the North Sea?three-dimensional problem into a two-dimensional one. Then three kinds of the formulations on surface water wave problems, i.e. the classical, the Lagrangian and the Hamiltonian, are described in outline.作者: 不能逃避 時(shí)間: 2025-3-23 13:52 作者: 搏斗 時(shí)間: 2025-3-23 21:09
https://doi.org/10.1007/978-1-349-09277-2he evolution of the modulated wave groups and for the generation of the second-order long waves. A Stuart-Landau equation obtained in the case of no spatial modulation is dynamically analyzed with respect to a steady current and a weakly oscillatory one.作者: Cloudburst 時(shí)間: 2025-3-24 01:59
https://doi.org/10.1007/978-1-349-09277-2aged flow system, leading to three new kinds of actions: the current wave action, the bottom wave action and the dissipative wave action. These actions can be applied to arbitrary depth over moving bottoms and ambient currents with a typical vertical structure, and probably have a widespread range of applications.作者: anaphylaxis 時(shí)間: 2025-3-24 03:37
https://doi.org/10.1007/978-1-349-09277-2 In addition, an operator representing the wide wave-current interactions is introduced to develop a hierarchy of the mild-slope equations for linear surface gravity waves with two-dimensional slowly-varying currents over uniformly-varying bottom topography.作者: 性冷淡 時(shí)間: 2025-3-24 10:31
The Mild-Slope Equations, In addition, an operator representing the wide wave-current interactions is introduced to develop a hierarchy of the mild-slope equations for linear surface gravity waves with two-dimensional slowly-varying currents over uniformly-varying bottom topography.作者: neutrophils 時(shí)間: 2025-3-24 13:04 作者: OFF 時(shí)間: 2025-3-24 17:45 作者: 尾隨 時(shí)間: 2025-3-24 22:34 作者: 磨坊 時(shí)間: 2025-3-25 01:52 作者: Ceremony 時(shí)間: 2025-3-25 07:15 作者: canvass 時(shí)間: 2025-3-25 10:11
https://doi.org/10.1007/978-1-349-09277-2 employing Hamilton’s canonical equations for surface waves, including the following special cases: the generalized nonlinear shallow-water equations of Airy, the generalized mild-slope equation, the dispersion relation for second-order Stokes waves and higher-order Boussinesq-type equations.作者: ILEUM 時(shí)間: 2025-3-25 12:46 作者: Exaggerate 時(shí)間: 2025-3-25 18:53
https://doi.org/10.1007/978-1-349-09277-2olution equations of Liu and Dingemans are pointed out and corrected. These modified equations are then extended to fourth-order with the stability analysis for uniform Stokes waves in which there exist certain fourth-order terms concerning the stability of finite depth waves, and to including the e作者: flimsy 時(shí)間: 2025-3-25 21:38
https://doi.org/10.1007/978-1-349-09277-2agnitude as the modulation one, the nonlinear resonant wave-current-bottom interactions are considered by using the WKBJ perturbation theory, resulting in synchronous resonance, superharmonic one, and subharmonic one which is investigated in detail to obtain a couple of the governing equations for t作者: insidious 時(shí)間: 2025-3-26 02:11 作者: tenosynovitis 時(shí)間: 2025-3-26 05:02
https://doi.org/10.1007/978-1-349-09277-2tion of wave numbers are presented to study linear gravity wave transformation over rigid, porous bottoms. The first specializes in that both the water and the porous layers consist of two kind of components: the slowly varying one whose horizontal length scale is longer than the surface wave length作者: 存在主義 時(shí)間: 2025-3-26 09:01 作者: Coeval 時(shí)間: 2025-3-26 16:40
https://doi.org/10.1007/978-1-349-09277-2 starting from the Navier-Stokes equations of motion of a viscous fluid including the Coriolis force, and taking account of the effects of moving bottoms. The theory extends the classical concept of wave action from the ideal averaged flow conservation system into the real dissipative dynamical aver作者: 粗鄙的人 時(shí)間: 2025-3-26 16:49 作者: 違法事實(shí) 時(shí)間: 2025-3-26 23:42 作者: hypertension 時(shí)間: 2025-3-27 01:29
Work Out Engineering Thermodynamics for comparison, concerning currents, shallow and deep water waves, and surface capillary waves. Fourthly, a third-order solution for surface gravity short-crested waves with a uniform current in finite depth is obtained, giving exhaustively explicit formulas for the wave force and moment exerted on作者: Repatriate 時(shí)間: 2025-3-27 05:45
Surface Capillary-Gravity Short-Crested Waves with a Current in Water of Finite Depth, for comparison, concerning currents, shallow and deep water waves, and surface capillary waves. Fourthly, a third-order solution for surface gravity short-crested waves with a uniform current in finite depth is obtained, giving exhaustively explicit formulas for the wave force and moment exerted on作者: 整頓 時(shí)間: 2025-3-27 12:53
Book 2009Latest editionamples showing how the theory works, and up-to-date techniques, all of which make it accessible to a wide variety of readers, especially senior undergraduate and graduate students in fluid mechanics, coastal and ocean engineering, physical oceanography and applied mathematics...Hu Huang is a profess作者: 演講 時(shí)間: 2025-3-27 17:08 作者: 碳水化合物 時(shí)間: 2025-3-27 20:16
Preliminaries, is briefly reviewed first, involving two important coastal current models: one-equation model—the mild-slope equation and its variants approximating the vertical structure of surface waves and averaging over variable depth; a shallow water approximation—the Boussinesq-type equations which reduce a 作者: AGOG 時(shí)間: 2025-3-27 22:35
Weakly Nonlinear Water Waves Propagating over Uneven Bottoms,olution equations of Liu and Dingemans are pointed out and corrected. These modified equations are then extended to fourth-order with the stability analysis for uniform Stokes waves in which there exist certain fourth-order terms concerning the stability of finite depth waves, and to including the e作者: oracle 時(shí)間: 2025-3-28 03:39
Resonant Interactions Between Weakly Nonlinear Stokes Waves and Ambient Currents and Uneven Bottomsagnitude as the modulation one, the nonlinear resonant wave-current-bottom interactions are considered by using the WKBJ perturbation theory, resulting in synchronous resonance, superharmonic one, and subharmonic one which is investigated in detail to obtain a couple of the governing equations for t作者: 裙帶關(guān)系 時(shí)間: 2025-3-28 09:04 作者: parallelism 時(shí)間: 2025-3-28 12:18 作者: recede 時(shí)間: 2025-3-28 14:49
Nonlinear Unified Equations over an Uneven Bottom, employing Hamilton’s canonical equations for surface waves, including the following special cases: the generalized nonlinear shallow-water equations of Airy, the generalized mild-slope equation, the dispersion relation for second-order Stokes waves and higher-order Boussinesq-type equations.
