標題: Titlebook: Atmospheric Tidal and Planetary Waves; Hans Volland Book 1988 Kluwer Academic Publishers 1988 Scale.Southern Oscillation.Storm.Tide.wind [打印本頁] 作者: 法官所用 時間: 2025-3-21 18:28
書目名稱Atmospheric Tidal and Planetary Waves影響因子(影響力)
書目名稱Atmospheric Tidal and Planetary Waves影響因子(影響力)學科排名
書目名稱Atmospheric Tidal and Planetary Waves網(wǎng)絡公開度
書目名稱Atmospheric Tidal and Planetary Waves網(wǎng)絡公開度學科排名
書目名稱Atmospheric Tidal and Planetary Waves被引頻次
書目名稱Atmospheric Tidal and Planetary Waves被引頻次學科排名
書目名稱Atmospheric Tidal and Planetary Waves年度引用
書目名稱Atmospheric Tidal and Planetary Waves年度引用學科排名
書目名稱Atmospheric Tidal and Planetary Waves讀者反饋
書目名稱Atmospheric Tidal and Planetary Waves讀者反饋學科排名
作者: 閃光你我 時間: 2025-3-21 20:48
https://doi.org/10.1007/978-94-007-7091-1at the equations of motion can be solved by separation of the variables (latitude, longitude, height, and time) and that the modal structure becomes an eigenvalue problem. In this chapter, we will discuss the eigenvalues of the individual modes and their horizontal structures.作者: 膽小鬼 時間: 2025-3-22 04:27 作者: 拱形大橋 時間: 2025-3-22 08:19 作者: Respond 時間: 2025-3-22 10:24
Horizontal Modal Structure,at the equations of motion can be solved by separation of the variables (latitude, longitude, height, and time) and that the modal structure becomes an eigenvalue problem. In this chapter, we will discuss the eigenvalues of the individual modes and their horizontal structures.作者: entice 時間: 2025-3-22 14:48 作者: GRILL 時間: 2025-3-22 18:56
Book 1988 indicates the preferred prejudice of many ionospheric physicists and geomagneticians in those days toward meteorology as a descriptive rather than an exact science, in spite of the presence of such giants as Carl Rossby and Hans Ertel.作者: Bumble 時間: 2025-3-22 23:34 作者: 休戰(zhàn) 時間: 2025-3-23 04:41
Internal Energy Sources and Sinks,bypass these difficulties by introducing secondary or internal ‘sources’ (or ‘sinks’). These internal sources are intended to parameterize the otherwise neglected processes like turbulence, latent heat, feedback between ground and atmosphere, etc.作者: explicit 時間: 2025-3-23 06:28
Nonlinear Wave Propagation,e types with mixed frequencies. Such interference cannot be described by the linear approximation. We want to estimate in this chapter the influence of the nonlinear terms in the wave equations on the excitation and propagation of global-scale waves.作者: 五行打油詩 時間: 2025-3-23 10:24
Planetary Waves, waves barely exceed the red meteorological noise, and statistical approaches are necessary to make them visible. However, individual planetary wave structures are noticeable in the middle atmosphere, and they become prominent features within the upper atmosphere.作者: eardrum 時間: 2025-3-23 17:02 作者: noxious 時間: 2025-3-23 19:03
Erlei M. Reis,Marcelo A. Carmonariable Brunt-V?is?l? frequency, this system can only be treated numerically. However, for an isothermal background atmosphere and constant dissipation terms, system (5.8) becomes a set of inhomogeneous linear differential equations with constant coefficients. Such system has analytical solutions.作者: 天文臺 時間: 2025-3-24 00:39 作者: 濃縮 時間: 2025-3-24 03:03 作者: ESO 時間: 2025-3-24 08:52
Tidal Waves,ds of one solar (lunar) day, or one year. They are excited directly or indirectly by solar thermal, orographic, or lunar gravitational forcing. Annual and semiannual variations of the weather related to the geometry of the Sun-Earth system are therefore part of tidal waves.作者: ellagic-acid 時間: 2025-3-24 13:42 作者: 平項山 時間: 2025-3-24 15:40 作者: 車床 時間: 2025-3-24 20:20 作者: 創(chuàng)造性 時間: 2025-3-25 01:21 作者: Hemiplegia 時間: 2025-3-25 03:58 作者: flammable 時間: 2025-3-25 11:04 作者: Interlocking 時間: 2025-3-25 14:02 作者: 音樂等 時間: 2025-3-25 17:38 作者: 整體 時間: 2025-3-25 20:01
Fusarium Head Blight in Latin Americamore convenient, however, to separate the atmospheric wave motions from a hypothetical motionless or stationary background atmosphere. The wind can be divided into a source-free (no divergence) and a curl-free (no vorticity) component.作者: Polydipsia 時間: 2025-3-26 02:14
https://doi.org/10.1007/978-94-007-7091-1 of the atmospheric gas is a complicated process that depends on the physical and chemical conditions of the atmosphere. Minor constituents like ozone or the ionospheric plasma play important roles in transferring solar energy into heat and momentum. Strictly speaking, one must solve a set of compli作者: 環(huán)形 時間: 2025-3-26 08:19
Martha Díaz de Ackermann,Man Mohan Kohlie to be taken into account. These indirect sources and sinks are a consequence of our limited ability to deal with the full complex system Earth-Ocean-Atmosphere on all scales of motion and to account for all physical and chemical processes in the multi-component atmospheric gas. Instead, we try to 作者: 捕鯨魚叉 時間: 2025-3-26 11:31 作者: 玷污 時間: 2025-3-26 13:23
Erlei M. Reis,Marcelo A. Carmona this, we have to solve the system of Equations (5.8). In the presence of a realistic background temperature with height dependent scale height and variable Brunt-V?is?l? frequency, this system can only be treated numerically. However, for an isothermal background atmosphere and constant dissipation作者: legitimate 時間: 2025-3-26 17:42
Erlei M. Reis,Marcelo A. Carmonanonlinear loss processes such as turbulence and eddy heat conduction by Rayleigh friction and Newtonian cooling. However, even without these loss processes, the waves interfere with each other via the nonlinear advection terms in the equations of motion. This nonlinear coupling gives rise to new wav作者: instructive 時間: 2025-3-26 23:10 作者: 刻苦讀書 時間: 2025-3-27 01:33 作者: FOVEA 時間: 2025-3-27 06:43 作者: NIL 時間: 2025-3-27 10:31 作者: 圓錐體 時間: 2025-3-27 16:04 作者: GOAD 時間: 2025-3-27 21:38
Hans VollandIncludes supplementary material: 作者: Glycogen 時間: 2025-3-27 22:44 作者: 死亡率 時間: 2025-3-28 02:53 作者: breadth 時間: 2025-3-28 08:03 作者: Mercantile 時間: 2025-3-28 11:42 作者: 河流 時間: 2025-3-28 16:55
Basic Equations,more convenient, however, to separate the atmospheric wave motions from a hypothetical motionless or stationary background atmosphere. The wind can be divided into a source-free (no divergence) and a curl-free (no vorticity) component.作者: 過于平凡 時間: 2025-3-28 19:06 作者: 憤怒事實 時間: 2025-3-28 23:44
Internal Energy Sources and Sinks,e to be taken into account. These indirect sources and sinks are a consequence of our limited ability to deal with the full complex system Earth-Ocean-Atmosphere on all scales of motion and to account for all physical and chemical processes in the multi-component atmospheric gas. Instead, we try to 作者: 國家明智 時間: 2025-3-29 05:15
Horizontal Modal Structure,iction and Newtonian cooling as dissipation terms. In this approximation, which often simulates observed wave structure reasonably well, the waves can be considered as decoupled from each other. It is then possible to find general solutions of any time dependent disturbance by linearly superimposing作者: CODA 時間: 2025-3-29 11:12 作者: 離開可分裂 時間: 2025-3-29 15:02
Nonlinear Wave Propagation,nonlinear loss processes such as turbulence and eddy heat conduction by Rayleigh friction and Newtonian cooling. However, even without these loss processes, the waves interfere with each other via the nonlinear advection terms in the equations of motion. This nonlinear coupling gives rise to new wav
