標(biāo)題: Titlebook: Geophysical Fluid Dynamics; Joseph Pedlosky Book 1982 Springer Science+Business Media New York 1982 Potential.circulation.dynamics.fluid d [打印本頁] 作者: Sediment 時(shí)間: 2025-3-21 16:35
書目名稱Geophysical Fluid Dynamics影響因子(影響力)
作者: 全部 時(shí)間: 2025-3-21 23:01
https://doi.org/10.1007/978-3-663-04792-6eral pattern of the oceanic circulation began to emerge. It is clear now that a time-averaged circulation pattern exists in all oceans, although its observations may be significantly distorted by the presence of energetic fluctuations.作者: FADE 時(shí)間: 2025-3-22 02:05 作者: Omnipotent 時(shí)間: 2025-3-22 08:08
Inviscid Shallow-Water Theory,mework adequate for the calculation of motions of large time and space scales. Furthermore, the method of analysis to be presented also can be generalized to the study of thermodynamically active fluids. The key technique of the analysis is the formulation of a . approximation scheme in which the geostrophic approximation is merely the first step.作者: 失望未來 時(shí)間: 2025-3-22 12:16
Book 1982ysical Sciences at The University of Chicago have taught for the past decade. Our purpose in developing a core curriculum was to provide to advanced undergraduates and entering graduate students a coherent and systematic introduction to the theory of geophysical fluid dynamics. The curriculum and th作者: 放肆的我 時(shí)間: 2025-3-22 12:57 作者: 放肆的我 時(shí)間: 2025-3-22 17:06
https://doi.org/10.1007/978-3-7091-7776-1ical motion and strongly affects the nature of the dynamics. It is also clear from the discussion in Section 2.9 that the vertical structure of the winds and currents is directly related to the presence and strength of horizontal density gradients by the thermal wind relation.作者: 沖突 時(shí)間: 2025-3-23 01:11 作者: 菊花 時(shí)間: 2025-3-23 04:00 作者: DAFT 時(shí)間: 2025-3-23 06:13 作者: 不知疲倦 時(shí)間: 2025-3-23 13:13 作者: crumble 時(shí)間: 2025-3-23 15:26
Die Verbreitung des elektrischen Kochens, any particular problem. However, the equations of motion are so complex that only rarely can exact solutions be found, and any method of approximation of the equations requires first an understanding of the broad, general, physical principles with which any approximation must be consistent.作者: 奇思怪想 時(shí)間: 2025-3-23 21:46 作者: STELL 時(shí)間: 2025-3-23 22:25 作者: GREEN 時(shí)間: 2025-3-24 02:38
https://doi.org/10.1007/978-3-663-04792-6are the dramatic elements of many a sea story. With the advent of the great age of navigation and exploration a more systematic description of the general pattern of the oceanic circulation began to emerge. It is clear now that a time-averaged circulation pattern exists in all oceans, although its o作者: FRET 時(shí)間: 2025-3-24 09:55
https://doi.org/10.1007/978-3-7091-7776-1rculations of both systems. Even the wind-driven oceanic circulation implicitly requires atmospheric buoyancy forces to produce the wind. In addition, the presence of a stable stratification in which heavier fluid underlies lighter, characteristic of both the atmosphere and the oceans, inhibits vert作者: 完成 時(shí)間: 2025-3-24 12:35 作者: insurgent 時(shí)間: 2025-3-24 18:28
https://doi.org/10.1007/978-3-662-54445-7ion that the time scale of the motion is large compared to ... This is not always sufficient, as the discussion of the Kelvin wave in Section 3.9 indicated. When the wavelength of the Kelvin wave is long compared to the deformation radius, the frequency is small compared to .. Yet the equation of mo作者: headlong 時(shí)間: 2025-3-24 22:12 作者: 狂亂 時(shí)間: 2025-3-25 01:08 作者: indicate 時(shí)間: 2025-3-25 04:58
Fundamentals, any particular problem. However, the equations of motion are so complex that only rarely can exact solutions be found, and any method of approximation of the equations requires first an understanding of the broad, general, physical principles with which any approximation must be consistent.作者: Gnrh670 時(shí)間: 2025-3-25 11:32 作者: 滔滔不絕地講 時(shí)間: 2025-3-25 15:25 作者: 大廳 時(shí)間: 2025-3-25 18:49 作者: 相符 時(shí)間: 2025-3-25 20:52
Elektrisches Messen nichtelektrischer Gr??ene persistent but spatially nonuniform solar heating. This input of energy produces a mechanical response, i.e., kinetic energy of the large-scale motion, and eventually this must be dissipated if a steady state—or at least a statistically stable average state of motion—is to be maintained. This requ作者: VOC 時(shí)間: 2025-3-26 03:14 作者: Peculate 時(shí)間: 2025-3-26 07:20
https://doi.org/10.1007/978-3-662-54445-7., that the scaling of the motion is isotropic horizontally. The low-frequency Kelvin wave is not horizontally isotropic, since its offshore scale is the deformation radius, which for low frequencies is small compared with the wavelength. In this chapter we consider some of the refinements to quasig作者: ornithology 時(shí)間: 2025-3-26 12:28 作者: 單色 時(shí)間: 2025-3-26 16:16
Friction and Viscous Flow,e persistent but spatially nonuniform solar heating. This input of energy produces a mechanical response, i.e., kinetic energy of the large-scale motion, and eventually this must be dissipated if a steady state—or at least a statistically stable average state of motion—is to be maintained. This requ作者: BLINK 時(shí)間: 2025-3-26 20:26 作者: Notify 時(shí)間: 2025-3-26 21:20
Ageostrophic Motion,., that the scaling of the motion is isotropic horizontally. The low-frequency Kelvin wave is not horizontally isotropic, since its offshore scale is the deformation radius, which for low frequencies is small compared with the wavelength. In this chapter we consider some of the refinements to quasig作者: Ballerina 時(shí)間: 2025-3-27 04:56
Preliminaries,perience has also shown that the recognition of the underlying dynamical concepts applicable to both the atmosphere and the oceans is an excellent starting point for the study of either. Geophysical fluid dynamics is the subject whose concerns are the fundamental dynamical concepts essential to an u作者: 我正派 時(shí)間: 2025-3-27 06:20
Fundamentals, any particular problem. However, the equations of motion are so complex that only rarely can exact solutions be found, and any method of approximation of the equations requires first an understanding of the broad, general, physical principles with which any approximation must be consistent.作者: 你不公正 時(shí)間: 2025-3-27 10:08
Inviscid Shallow-Water Theory,oses to our consideration of this physical system. It is first of all simple enough so that the issues raised by the problem of geostrophic degeneracy can be dealt with directly without the need to simultaneously treat the complexities of the thermodynamics of a density-stratified fluid. The first g作者: DOTE 時(shí)間: 2025-3-27 15:36
Friction and Viscous Flow,eak, almost everywhere, when compared with the Coriolis acceleration and the pressure gradient. Friction rarely upsets the geostrophic balance to lowest order. Indeed, for many flows it is probably also true that the dissipative time scale is long compared to the advective time scale, i.e., that the作者: 瘙癢 時(shí)間: 2025-3-27 18:01 作者: 形上升才刺激 時(shí)間: 2025-3-28 01:33 作者: bromide 時(shí)間: 2025-3-28 02:39 作者: APEX 時(shí)間: 2025-3-28 08:04
Ageostrophic Motion,ion that the time scale of the motion is large compared to ... This is not always sufficient, as the discussion of the Kelvin wave in Section 3.9 indicated. When the wavelength of the Kelvin wave is long compared to the deformation radius, the frequency is small compared to .. Yet the equation of mo作者: WAX 時(shí)間: 2025-3-28 11:56
,A Contribution to Keller’s jacobian conjecture,f the mapping (P,Q), then each of the coordinates P and Q has at most d + 2 zeros at infinity. There have been obtained some equations connecting the homogeneous components of the polynomials P and Q.作者: Occipital-Lobe 時(shí)間: 2025-3-28 16:11
