標題: Titlebook: Dynamics of Internal Gravity Waves in the Ocean; Yu. Z. Miropol’sky,O. D. Shishkina Book 2001 Springer Science+Business Media Dordrecht 20 [打印本頁] 作者: BRISK 時間: 2025-3-21 17:58
書目名稱Dynamics of Internal Gravity Waves in the Ocean影響因子(影響力)
書目名稱Dynamics of Internal Gravity Waves in the Ocean影響因子(影響力)學科排名
書目名稱Dynamics of Internal Gravity Waves in the Ocean網(wǎng)絡公開度
書目名稱Dynamics of Internal Gravity Waves in the Ocean網(wǎng)絡公開度學科排名
書目名稱Dynamics of Internal Gravity Waves in the Ocean被引頻次
書目名稱Dynamics of Internal Gravity Waves in the Ocean被引頻次學科排名
書目名稱Dynamics of Internal Gravity Waves in the Ocean年度引用
書目名稱Dynamics of Internal Gravity Waves in the Ocean年度引用學科排名
書目名稱Dynamics of Internal Gravity Waves in the Ocean讀者反饋
書目名稱Dynamics of Internal Gravity Waves in the Ocean讀者反饋學科排名
作者: 責任 時間: 2025-3-21 20:22
Stephen Spender: a traveller through Japanatistical methods of the description of internal waves’ field as well as the methods of interpretation of evidence are valid only for small amplitude (linear and weakly nonlinear) waves. When natural internal waves have strong slopes and nonlinear effects take place, traditional spectral and correlation statistical methods are hardly applicable.作者: 積極詞匯 時間: 2025-3-22 03:22 作者: CLOWN 時間: 2025-3-22 05:54
Pronatalism and Women’s Equality Policies velocity fields. A brief overview of the other sources of the generation of internal waves is given in the conclusions of the chapter. Specific questions of wave generation by underwater earthquakes, tidal flows, and bottom obstacles are presented in [49], [179] and therefore are not considered here.作者: 是比賽 時間: 2025-3-22 10:40
Basic Sources of Internal Waves Generation in the Ocean velocity fields. A brief overview of the other sources of the generation of internal waves is given in the conclusions of the chapter. Specific questions of wave generation by underwater earthquakes, tidal flows, and bottom obstacles are presented in [49], [179] and therefore are not considered here.作者: 徹底明白 時間: 2025-3-22 15:58
G S Fraser: a Westerner’s analysis of ta from laboratory experiments on the study of internal waves are given. Hypothetical mechanisms of internal waves’ breaking and dissipation, based on the evidence, are discussed in the final Section 12.5.作者: 徹底明白 時間: 2025-3-22 20:30
Basic Experimental Facts of Internal Waves’ Behaviour in the Oceanta from laboratory experiments on the study of internal waves are given. Hypothetical mechanisms of internal waves’ breaking and dissipation, based on the evidence, are discussed in the final Section 12.5.作者: RACE 時間: 2025-3-23 00:37
On Statistical Description of Natural Internal Waves Dataatistical methods of the description of internal waves’ field as well as the methods of interpretation of evidence are valid only for small amplitude (linear and weakly nonlinear) waves. When natural internal waves have strong slopes and nonlinear effects take place, traditional spectral and correlation statistical methods are hardly applicable.作者: 他姓手中拿著 時間: 2025-3-23 01:37 作者: 解開 時間: 2025-3-23 07:05 作者: Excitotoxin 時間: 2025-3-23 10:55
Childcare Policies and Programmesopagation of free infinitesimal internal waves is studied in Section 3.5. The influence of the Earth’s rotation (taking into account all components of the Coriolis force) on the propagation of free internal waves is considered in Section 3.6.作者: 使絕緣 時間: 2025-3-23 17:36 作者: fulcrum 時間: 2025-3-23 22:03 作者: GULLY 時間: 2025-3-24 00:28 作者: 鳴叫 時間: 2025-3-24 03:55 作者: FLINT 時間: 2025-3-24 06:39
Propagation of Weakly Nonlinear Internal Wave Packets in the Oceangly in the vertical direction. The theory of the formation of oceanic fine structure, based on this phenomenon, is proposed. A rather good agreement between the evidence and numerical results for certain of some of the stratification profiles was obtained. In Section 9.4 propagation of a weakly nonl作者: 教義 時間: 2025-3-24 14:33
https://doi.org/10.1007/978-94-017-1325-2Ocean; Oceanography; differential equation; dynamics; waves; fluid- and aerodynamics作者: 慢慢沖刷 時間: 2025-3-24 18:47
978-90-481-5692-4Springer Science+Business Media Dordrecht 2001作者: Visual-Field 時間: 2025-3-24 22:27
Atmospheric and Oceanographic Sciences Libraryhttp://image.papertrans.cn/e/image/284106.jpg作者: Directed 時間: 2025-3-25 00:35
How Do We Know about Past Lives?Investigations in the field of internal gravity waves has occupied one of the central places in oceanology in recent years. The topicality of the problems is caused first of all by propagation of internal wave motions in the entire depth of the World Ocean, and, in this connection, by their important role in all oceanic dynamic phenomena.作者: 慌張 時間: 2025-3-25 05:10 作者: Insubordinate 時間: 2025-3-25 10:32 作者: 脫落 時間: 2025-3-25 14:08 作者: 牽連 時間: 2025-3-25 17:38 作者: 噴油井 時間: 2025-3-25 20:17
Brief Information about Oceanic ThermohydrodynamicsIn this chapter the principles of oceanic thermohydrodynamics are presented briefly. For the relatively short internal waves with length scales less than 100 km, considered in this hook, it is obviously possible to neglect the radius of the Earth restricting the local description.作者: neutralize 時間: 2025-3-26 03:43 作者: MITE 時間: 2025-3-26 05:51
Resonant Interactions of Wave Triads and Kinetic Equation for Oceanic Internal Waves’ SpectrumNonlinear effects while internal waves propagate in the ocean are caused not only by the self-modulation of almost monochromatic internal wave packets, but also by the interaction of internal waves with different wave numbers, frequencies and mode numbers.作者: 拘留 時間: 2025-3-26 09:54
Equations of the Theory of Internal Wavesf oceanic thermodynamics derived in Chapter 1. A list of different forms of these equations for special cases plane (twodimensional) stationary and nonstationary problems, equations linearized relative to the state of rest and to background flow — is given here for convenience.作者: GROUP 時間: 2025-3-26 14:31 作者: 辯論的終結 時間: 2025-3-26 18:55
Propagation of Internal Waves in Horizontally Inhomogeneous Oceanaracteristic horizontal inhomogeneities are: bottom unevenness; horizontal inhomogeneities of the density field; and horizontal variations of the mean flows. The influence of these phenomena on internal waves’ propagation will be studied in this chapter.作者: 懶鬼才會衰弱 時間: 2025-3-26 23:13 作者: 感染 時間: 2025-3-27 03:59
Childcare Policies and Programmesocean. A detailed analysis of the basic boundary value problem for amplitude functions of these internal waves for a finite depth is given in Section 3.1. Examples of solutions of the basic boundary value problem for typical vertically undisturbed density distributions in the ocean are presented in 作者: jagged 時間: 2025-3-27 08:16 作者: DOTE 時間: 2025-3-27 13:21 作者: 偽書 時間: 2025-3-27 17:14 作者: FLOAT 時間: 2025-3-27 19:59
G S Fraser: a Westerner’s analysis of ts own analysis. The first is the propagation of internal waves in shallow water (e.g., in a shallow sea like the Baltic Sea) when the wavelength . considerably exceeds the sea’s depth .. In this case equations of internal waves dynamics are reduced to the Korteweg-de Vries equation (KdV) (see a rev作者: 正常 時間: 2025-3-27 23:07 作者: meretricious 時間: 2025-3-28 03:36 作者: 衰老 時間: 2025-3-28 08:11
G S Fraser: a Westerner’s analysis of of basic properties of frequency and spatial spectra of internal waves measured in the ocean is given at the beginning. Then local properties of measured short period internal waves (in particular, wave packets) are analyzed. One of the important characteristics of an internal wave field is the prob作者: Conflict 時間: 2025-3-28 11:50
Dynamics of Internal Gravity Waves in the Ocean978-94-017-1325-2Series ISSN 1383-8601 Series E-ISSN 2215-162X 作者: DEBT 時間: 2025-3-28 16:57
How Do We Know about Past Lives?f oceanic thermodynamics derived in Chapter 1. A list of different forms of these equations for special cases plane (twodimensional) stationary and nonstationary problems, equations linearized relative to the state of rest and to background flow — is given here for convenience.作者: 昏睡中 時間: 2025-3-28 21:06 作者: 擦掉 時間: 2025-3-28 23:03
Pronatalism and Women’s Equality Policiesaracteristic horizontal inhomogeneities are: bottom unevenness; horizontal inhomogeneities of the density field; and horizontal variations of the mean flows. The influence of these phenomena on internal waves’ propagation will be studied in this chapter.作者: 糾纏 時間: 2025-3-29 06:35
Equations of the Theory of Internal Wavesf oceanic thermodynamics derived in Chapter 1. A list of different forms of these equations for special cases plane (twodimensional) stationary and nonstationary problems, equations linearized relative to the state of rest and to background flow — is given here for convenience.作者: 紳士 時間: 2025-3-29 09:11
Linear Theory of Propagation of Internal Waves in the Undisturbed Horizontally Homogeneous Oceanocean. A detailed analysis of the basic boundary value problem for amplitude functions of these internal waves for a finite depth is given in Section 3.1. Examples of solutions of the basic boundary value problem for typical vertically undisturbed density distributions in the ocean are presented in 作者: 周年紀念日 時間: 2025-3-29 14:27
Shear Flow Influence on Internal Waves Propagationhe seasonal thermocline zone and may strongly influence the internal waves’ dynamics. If a characteristic period of a shear flow variation is considerably greater than the internal waves’ period and the horizontal variations are small, then the flow may be considered to be stationary and horizontall作者: braggadocio 時間: 2025-3-29 17:04 作者: 啞劇 時間: 2025-3-29 21:47
Basic Sources of Internal Waves Generation in the Ocean ocean’s bottom (during underwater earthquakes), by tidal forces etc.. Nonlinear mechanisms of internal waves generation, e.g., resonant interaction of surface waves for a flow over large bottom obstacles, are quite important. The generation of internal waves by oscillations of wind and atmospheric 作者: sebaceous-gland 時間: 2025-3-30 00:07 作者: 走調 時間: 2025-3-30 04:18
Propagation of Weakly Nonlinear Internal Wave Packets in the Oceansting from the viewpoint of oceanology is that of a weakly nonlinear internal wave packet with the mode structure generating velocity, density, and pressure fields which do not vanish when averaged over the wave period. In Section 9.1 the main characteristics of such fields are obtained. In Section 作者: Gorilla 時間: 2025-3-30 09:59 作者: GOAD 時間: 2025-3-30 13:14
Basic Experimental Facts of Internal Waves’ Behaviour in the Oceanof basic properties of frequency and spatial spectra of internal waves measured in the ocean is given at the beginning. Then local properties of measured short period internal waves (in particular, wave packets) are analyzed. One of the important characteristics of an internal wave field is the prob作者: CLAY 時間: 2025-3-30 19:47
