作者: bronchodilator 時(shí)間: 2025-3-21 22:46
operties of the atmospheric boundary layer are discussed, with a focus on the interaction between turbulence and mean flows. This is followed by a detailed look at the global atmospheric circulation, highlighting its control by Rossby waves and grav978-3-662-63940-5978-3-662-63941-2作者: Intact 時(shí)間: 2025-3-22 03:03
Allgemeine Anatomie des Bewegungsapparates,es the fundamental wave motions of an atmosphere at rest, moves on to the description of the interaction between mesoscale gravity waves and a synoptic-scale flow, and finally demonstrates how that theory can explain the observed gravity-wave effects in the middle atmosphere.作者: MUTED 時(shí)間: 2025-3-22 07:30
Textbook 2022by means of baroclinic instability. The specific properties of the atmospheric boundary layer are discussed, with a focus on the interaction between turbulence and mean flows. This is followed by a detailed look at the global atmospheric circulation, highlighting its control by Rossby waves and grav作者: Accomplish 時(shí)間: 2025-3-22 11:52 作者: 鐵塔等 時(shí)間: 2025-3-22 12:52
Hans-Joachim Appell,Christiane Stang-Vossnerality but rather focus on the . and derive the corresponding quasigeostrophic theory. This will enable us to describe not only the . but also the generation of synoptic-scale extratropical weather by ..作者: inquisitive 時(shí)間: 2025-3-22 17:04
Funktionelle Anatomie der Organsysteme,lation, zonal mean of wind and temperature, and waves arrange themselves as observed. Important open questions still remain, but the theory of atmospheric dynamics can explain a lot. We will here first sketch a few essentials of the empirical findings, then discuss the circulation in the tropics, and finally we will consider the midlatitudes.作者: 食品室 時(shí)間: 2025-3-22 22:17 作者: 輕率的你 時(shí)間: 2025-3-23 02:16 作者: resuscitation 時(shí)間: 2025-3-23 06:46 作者: 隼鷹 時(shí)間: 2025-3-23 11:38 作者: 補(bǔ)助 時(shí)間: 2025-3-23 14:28
Elementary Thermodynamics and Energetics of Dry Air,d by these equations but not predicted by them is .. The prediction of pressure is one of the goals of this chapter. For this purpose a predictive equation for . is derived. Using the . for air, pressure can be obtained from density and temperature.作者: rectum 時(shí)間: 2025-3-23 21:51 作者: 思鄉(xiāng)病 時(shí)間: 2025-3-24 00:56 作者: 輕推 時(shí)間: 2025-3-24 02:56
The Planetary Boundary Layer,the planetary boundary layer. That layer is the part of the atmosphere where the transition from the boundary condition . to the discussed solutions of the free atmosphere is taking place via the effects of molecular and turbulent friction.作者: 誤傳 時(shí)間: 2025-3-24 06:51 作者: 關(guān)節(jié)炎 時(shí)間: 2025-3-24 12:40
Gravity Waves and Their Impact on the Atmospheric Flow,sby waves. In the stratosphere above the tropopause and especially in the mesosphere above the stratopause at about 50?km altitude, however, mesoscale gravity waves are a factor not to be ignored. Gravity waves are emitted by various processes in the troposphere, most prominently flow over mountains作者: aphasia 時(shí)間: 2025-3-24 17:19
https://doi.org/10.1007/978-3-642-68593-4also require knowledge of the evolving pressure distribution. The prediction of the latter, using a prognostic equation for the temperature and the thermodynamic equation of state, will be discussed later.作者: 粗野 時(shí)間: 2025-3-24 19:19 作者: 不透明 時(shí)間: 2025-3-25 02:04 作者: hallow 時(shí)間: 2025-3-25 04:01
Hans-Joachim Appell,Christiane Stang-Vossanishing vertical gradients in the horizontal wind are not realistic. These will now be dropped. We will not, however, treat the atmosphere in full generality but rather focus on the . and derive the corresponding quasigeostrophic theory. This will enable us to describe not only the . but also the g作者: organic-matrix 時(shí)間: 2025-3-25 11:03 作者: 搖曳 時(shí)間: 2025-3-25 13:17 作者: 蜿蜒而流 時(shí)間: 2025-3-25 18:38 作者: Carbon-Monoxide 時(shí)間: 2025-3-25 23:58 作者: 僵硬 時(shí)間: 2025-3-26 00:44 作者: Opponent 時(shí)間: 2025-3-26 07:47
Hans-Joachim Appell,Christiane Stang-VossThe?following questions are central in studies of the global circulation:作者: 一加就噴出 時(shí)間: 2025-3-26 08:49
Hans-Joachim Appell,Christiane Stang-VossVector analysis is an important tool of fluid mechanics. Here we summarize some of its important elements.作者: 通便 時(shí)間: 2025-3-26 13:07 作者: 容易懂得 時(shí)間: 2025-3-26 18:56 作者: 直覺沒有 時(shí)間: 2025-3-27 00:33
The Interaction Between Rossby Waves and the Mean Flow,The?following questions are central in studies of the global circulation:作者: 脾氣暴躁的人 時(shí)間: 2025-3-27 04:38 作者: evasive 時(shí)間: 2025-3-27 07:41 作者: 衣服 時(shí)間: 2025-3-27 09:47 作者: 混雜人 時(shí)間: 2025-3-27 17:20 作者: MANIA 時(shí)間: 2025-3-27 21:06 作者: 表示向前 時(shí)間: 2025-3-27 22:01 作者: 罐里有戒指 時(shí)間: 2025-3-28 02:24
Strukturierter Erreichbarkeitsgraph,d by these equations but not predicted by them is .. The prediction of pressure is one of the goals of this chapter. For this purpose a predictive equation for . is derived. Using the . for air, pressure can be obtained from density and temperature.作者: harpsichord 時(shí)間: 2025-3-28 08:31 作者: 惡意 時(shí)間: 2025-3-28 10:28 作者: Devastate 時(shí)間: 2025-3-28 17:03
The Basic Equations of Atmospheric Motion,also require knowledge of the evolving pressure distribution. The prediction of the latter, using a prognostic equation for the temperature and the thermodynamic equation of state, will be discussed later.作者: Orchiectomy 時(shí)間: 2025-3-28 20:17 作者: eucalyptus 時(shí)間: 2025-3-28 23:33 作者: 陰謀小團(tuán)體 時(shí)間: 2025-3-29 03:46
The Planetary Boundary Layer,the planetary boundary layer. That layer is the part of the atmosphere where the transition from the boundary condition . to the discussed solutions of the free atmosphere is taking place via the effects of molecular and turbulent friction.作者: 膠水 時(shí)間: 2025-3-29 09:28 作者: 連接 時(shí)間: 2025-3-29 13:16 作者: FAZE 時(shí)間: 2025-3-29 19:02
Conducting Polymers, Fundamentals and ApplicationsA Practical Approach
