標(biāo)題: Titlebook: Dynamics of the Equatorial Ocean; John P. Boyd Book 2018 Springer-Verlag GmbH Germany 2018 El Nino/Southern Oscillation.Coastally Trapped [打印本頁] 作者: Taft 時(shí)間: 2025-3-21 18:34
書目名稱Dynamics of the Equatorial Ocean影響因子(影響力)
書目名稱Dynamics of the Equatorial Ocean影響因子(影響力)學(xué)科排名
書目名稱Dynamics of the Equatorial Ocean網(wǎng)絡(luò)公開度
書目名稱Dynamics of the Equatorial Ocean網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Dynamics of the Equatorial Ocean被引頻次
書目名稱Dynamics of the Equatorial Ocean被引頻次學(xué)科排名
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書目名稱Dynamics of the Equatorial Ocean年度引用學(xué)科排名
書目名稱Dynamics of the Equatorial Ocean讀者反饋
書目名稱Dynamics of the Equatorial Ocean讀者反饋學(xué)科排名
作者: 山崩 時(shí)間: 2025-3-21 23:47 作者: crucial 時(shí)間: 2025-3-22 03:45 作者: GRATE 時(shí)間: 2025-3-22 05:09
,The “Long Wave” Approximation & Geostrophy,t that has been extremely useful in low latitude dynamics. The “l(fā)ong wave” approximation, which might equally well be dubbed the “l(fā)ow frequency” or “meridional geostrophy” approximation, filters gravity waves while retaining Kelvin and Rossby waves. The key assumption is that there is geostrophic ba作者: Emg827 時(shí)間: 2025-3-22 09:08 作者: 菊花 時(shí)間: 2025-3-22 14:22
Response of the Equatorial Ocean to Periodic Forcing, the theory of the ocean response to a periodically-varying wind stress. Special emphasis is given to low frequency forcing and the use of the low frequency/meridional geostrophy approximation to analyze it.作者: 菊花 時(shí)間: 2025-3-22 17:43
Impulsive Forcing and Spin-Up,be formally solved by Laplace transform integrals (multiplied by the usual Hermite functions). Although these transform integrals must evaluated numerically, it is still possible to analyze the oceanic response to jumps in the wind. The work of Anderson and Rowlands (J Mar Res 34(3):295–312, 1976) [作者: intertwine 時(shí)間: 2025-3-23 00:30
Yoshida Jet and Theories of the Undercurrent,he f-plane and then on the equatorial plane. In contrast to the midlatitudes where the steady-state flow is a geostrophically balanced jet . to the wind, Yoshida showed, through an infinite Hermite series with explicit, analytical coefficients, that a zonal wind stress would yield a zonal equatorial作者: 要素 時(shí)間: 2025-3-23 02:49
Stratified Models of Mean Currents,tion theorists. In this chapter, stratification and viscosity are added to the shallow water jets found by Yoshida. The models of McCreary and McPhaden are ancient and cannot fit observations as well as the ever-changing succession of ocean general circulation models. Yet they are well worth a caref作者: musicologist 時(shí)間: 2025-3-23 08:12 作者: 消息靈通 時(shí)間: 2025-3-23 12:34 作者: 溫和女孩 時(shí)間: 2025-3-23 16:19 作者: 撕裂皮肉 時(shí)間: 2025-3-23 21:10 作者: Offensive 時(shí)間: 2025-3-24 02:04
Nonmodal Instability,ments show that nonmodal perturbations must always decay as .. However, plane Couette flow is always unstable in the laboratory in a broad range of Reynolds numbers where all normal modes are stable. Orr pointed out in 1907 that nonmodal disturbances may exhibit a transient growth that may push thei作者: byline 時(shí)間: 2025-3-24 05:51
Nonlinear Equatorial Waves,litude waves and likewise the vertical structure of a baroclinic eigenfunction. East-west, equatorial waves are free both to propagate and also to evolve; the zonal-and-time amplitude function, .(.,?.), satisfies one of several generic PDEs or PDE systems. Each one-space-dimensional PDE is derived b作者: ventilate 時(shí)間: 2025-3-24 09:25
Nonlinear Wavepackets and Nonlinear Schroedinger Equation,initesimal amplitude sine wave) multiplied by an “envelope” or “modulation” function that slowly varies in both space and time and satisfies the cubically-Nonlinear Schroedinger (NLS) equation. The coefficient of the nonlinear terms, the “Landau constant”, has many discrete singularities at various 作者: 單片眼鏡 時(shí)間: 2025-3-24 12:58
Producing Adult Readers: 1930–50d the equator. Jets parallel to, rather than perpendicular to, the mean wind arise at low latitudes. Surface jets in opposite directions alternate in latitude. Vertically, jets of alternating signs are stacked one atop the other in the abyssal equatorial ocean like a stack of pancakes. The equatoria作者: HPA533 時(shí)間: 2025-3-24 18:39
U.S. Web Accessibility Law in Depthly analyzed for estimated error, culminating in a full four-dimensional separation of variables. The general solution to these approximate equations is a superposition of normal modes. Each mode is the product of four one-dimensional factors. The latitudinal structure of the modes is a Hermite funct作者: BACLE 時(shí)間: 2025-3-24 19:49 作者: diskitis 時(shí)間: 2025-3-25 01:46
Overview of Accessible Technologiest that has been extremely useful in low latitude dynamics. The “l(fā)ong wave” approximation, which might equally well be dubbed the “l(fā)ow frequency” or “meridional geostrophy” approximation, filters gravity waves while retaining Kelvin and Rossby waves. The key assumption is that there is geostrophic ba作者: BRUNT 時(shí)間: 2025-3-25 06:48 作者: Coterminous 時(shí)間: 2025-3-25 08:13 作者: CRUC 時(shí)間: 2025-3-25 11:50 作者: dermatomyositis 時(shí)間: 2025-3-25 17:44 作者: 擁護(hù)者 時(shí)間: 2025-3-25 21:03 作者: Commission 時(shí)間: 2025-3-26 03:25 作者: Liability 時(shí)間: 2025-3-26 07:58 作者: 離開真充足 時(shí)間: 2025-3-26 11:19
Module Design and Implementation, if ., that is, if there is nonzero latitudinal shear at the equator. Inertial instability is the primary suspect in the formation of (“pancake”) alternating jets in the tropical stratosphere and of deep internal jets in the equatorial ocean. Particle models, Taylor-Couette flow, and instability cri作者: Excitotoxin 時(shí)間: 2025-3-26 14:19
Taming the Device with the Game Enginetability for all ., however small. A power series in . is useless because . which goes to zero faster than any finite power of . as .. To capture “beyond-all-orders” effects, Hermité-Padé approximants, exponential asymptotics and numerical methods that loop off the real axis are applied to a hierarc作者: 愛哭 時(shí)間: 2025-3-26 20:21
Windows Mobile Game Developmentments show that nonmodal perturbations must always decay as .. However, plane Couette flow is always unstable in the laboratory in a broad range of Reynolds numbers where all normal modes are stable. Orr pointed out in 1907 that nonmodal disturbances may exhibit a transient growth that may push thei作者: 鞭打 時(shí)間: 2025-3-26 20:56 作者: FLIT 時(shí)間: 2025-3-27 01:12 作者: 保守 時(shí)間: 2025-3-27 05:55
John P. BoydContains appendices for illustrating special cases.Treats the important semiannual and annual cycles in the tropic sea.Includes complementary information to assist the reader in understanding the diff作者: 會犯錯(cuò)誤 時(shí)間: 2025-3-27 12:33
http://image.papertrans.cn/e/image/284206.jpg作者: Aboveboard 時(shí)間: 2025-3-27 13:48 作者: epinephrine 時(shí)間: 2025-3-27 17:55 作者: MAOIS 時(shí)間: 2025-3-28 00:42
Reflections and Boundaries,of the reflection of equatorial waves from straight boundaries aligned with a meridian. Although the equatorial oceans are effectively unbounded north and south, normal modes and quasi-normal modes do exist and are analyzed in the middle of the chapter. The final part is reflection from irregular boundaries and scattering from islands.作者: 做作 時(shí)間: 2025-3-28 05:07
Response of the Equatorial Ocean to Periodic Forcing, the theory of the ocean response to a periodically-varying wind stress. Special emphasis is given to low frequency forcing and the use of the low frequency/meridional geostrophy approximation to analyze it.作者: Alpha-Cells 時(shí)間: 2025-3-28 06:49 作者: Autobiography 時(shí)間: 2025-3-28 14:18
https://doi.org/10.1007/978-3-662-55476-0El Nino/Southern Oscillation; Coastally Trapped Waves; Equatorial Ocean; Nonlinear EquatorialWaves; Deep作者: 駭人 時(shí)間: 2025-3-28 16:30 作者: 斗志 時(shí)間: 2025-3-28 20:13
https://doi.org/10.1007/978-1-4302-0323-0of the reflection of equatorial waves from straight boundaries aligned with a meridian. Although the equatorial oceans are effectively unbounded north and south, normal modes and quasi-normal modes do exist and are analyzed in the middle of the chapter. The final part is reflection from irregular boundaries and scattering from islands.作者: osteopath 時(shí)間: 2025-3-29 01:56 作者: 母豬 時(shí)間: 2025-3-29 06:32
Magazine: My, What a Classy riven waves deep into the interior. However, the jump in density at the main thermocline will reflect waves. Deep penetrating waves, on the other hand, will bounce off the bottom. Using ideas borrowed from quantum scattering, vertical beams are analyzed through a mix of theory and number-crunching.作者: 樹木中 時(shí)間: 2025-3-29 10:00
Stable Linearized Waves in a Shear Flow,shear problems can also be attacked analytically by multiple scales perturbation theory. The horrendous algebra usual to this approach is enormously reduced by invocation of wave-mean flow conservations laws.作者: Nibble 時(shí)間: 2025-3-29 14:45 作者: 過分自信 時(shí)間: 2025-3-29 17:03
Nonlinear Equatorial Waves,sby waves are weakly dispersive, and only weakly dispersive, with or without mean currents, and the latitudinally symmetric modes are governed by the KdV equation, too. The . Rossby soliton is stable even for large amplitude, a pair of contra-rotating anticyclones that resembles middle latitude vort作者: Anthropoid 時(shí)間: 2025-3-29 20:35 作者: abreast 時(shí)間: 2025-3-30 00:20 作者: ANIM 時(shí)間: 2025-3-30 04:24
Windows Mobile Game Developmentrepresent. How do these scenarios play out in the tropics? Boyd and Christidis have made a tentative beginning at answering this question, but this chapter is less a review of equatorial dynamics than a research agenda.作者: surmount 時(shí)間: 2025-3-30 10:37 作者: 燕麥 時(shí)間: 2025-3-30 16:03 作者: Flatus 時(shí)間: 2025-3-30 20:07 作者: 類人猿 時(shí)間: 2025-3-30 21:55
An Observational Overview of the Equatorial Ocean,ional phenomena are reviewed in this introductory chapter to lay a foundation for what follows. The alternating surface jets, deep internal jets, seasonal reversals of the Somali Current with the monsoons, upwelling in the Gulf of Guinea and the coupled hemispheric and oceanic oscillation of huge climatic impact, ENSO, are all briefly surveyed.作者: Asparagus 時(shí)間: 2025-3-31 01:53 作者: 引水渠 時(shí)間: 2025-3-31 06:51 作者: mechanical 時(shí)間: 2025-3-31 12:02
Basic Equations and Normal Modes,ion or the sum of a pair of Hermite functions. The vertical structure functions are the eigenmodes of the vertical structure equation. The normal mode is the product of a factor of latitude multiplied by a function of depth . only and lastly multiplied by ..作者: 是他笨 時(shí)間: 2025-3-31 15:09
,The “Long Wave” Approximation & Geostrophy,lance in the latitudinal momentum equation only. This chapter also discusses the separation between the high and low frequency waves and the usefulness of this separation for initialization of equatorial numerical models.
