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標(biāo)題: Titlebook: Atmospheric Thermodynamics; J. V. Iribarne,W. L. Godson Book 1973 Springer Science+Business Media Dordrecht 1973 thermodynamics [打印本頁]

作者: Buren    時間: 2025-3-21 16:22
書目名稱Atmospheric Thermodynamics影響因子(影響力)




書目名稱Atmospheric Thermodynamics影響因子(影響力)學(xué)科排名




書目名稱Atmospheric Thermodynamics網(wǎng)絡(luò)公開度




書目名稱Atmospheric Thermodynamics網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Atmospheric Thermodynamics被引頻次




書目名稱Atmospheric Thermodynamics被引頻次學(xué)科排名




書目名稱Atmospheric Thermodynamics年度引用




書目名稱Atmospheric Thermodynamics年度引用學(xué)科排名




書目名稱Atmospheric Thermodynamics讀者反饋




書目名稱Atmospheric Thermodynamics讀者反饋學(xué)科排名





作者: aerial    時間: 2025-3-21 20:30
The Second Principle of Thermodynamics,s process might actually occur at all. It is the second principle that faces this problem and provides at the same time a rigorous criterion to decide when a system is in a state of thermodynamic equilibrium.
作者: FOVEA    時間: 2025-3-22 01:05
Water-Air Systems, structure of the system is implicit in them. Any of the four equivalent equations is a joint expression of the first and second principles, and therefore contains all that thermodynamics can say about closed systems, except as regards the third principle. Furthermore, while we deal with systems tha
作者: 好開玩笑    時間: 2025-3-22 06:14
Aerological Diagrams,use is made of special thermodynamic diagrams, or .. The observational data to be represented are obtained from soundings, and consist of sets of values of temperature, pressure, and humidity (e.g., relative humidity).
作者: 善辯    時間: 2025-3-22 10:08

作者: DRILL    時間: 2025-3-22 13:54
Vertical Stability,rmodynamic equilibrium; for instance, the vertical gradient of temperature will imply vertical heat conduction. In the real atmosphere heat will also be lost or gained by radiative processes. If vertical equilibrium is not prevalent, we should consider a third type of heat transport process: turbule
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作者: SHRIK    時間: 2025-3-23 07:31
Dimensions of Self-affine Sets: A Survey,use is made of special thermodynamic diagrams, or .. The observational data to be represented are obtained from soundings, and consist of sets of values of temperature, pressure, and humidity (e.g., relative humidity).
作者: 性別    時間: 2025-3-23 10:03
Vibrations with Two Degrees of Freedom,several general aspects related to the vertical stratification of the atmosphere and then, in the next chapter, to the vertical stability of the atmosphere. By ‘vertical’ we mean that the atmosphere will be considered above a certain location on the Earth’s surface, generally taking into account nei
作者: 火花    時間: 2025-3-23 14:28
An Introduction to Automatic Control,rmodynamic equilibrium; for instance, the vertical gradient of temperature will imply vertical heat conduction. In the real atmosphere heat will also be lost or gained by radiative processes. If vertical equilibrium is not prevalent, we should consider a third type of heat transport process: turbule
作者: hazard    時間: 2025-3-23 18:26

作者: 他日關(guān)稅重重    時間: 2025-3-24 01:09
The Second Principle of Thermodynamics,s process might actually occur at all. It is the second principle that faces this problem and provides at the same time a rigorous criterion to decide when a system is in a state of thermodynamic equilibrium.
作者: 殘廢的火焰    時間: 2025-3-24 06:19
Aerological Diagrams,use is made of special thermodynamic diagrams, or .. The observational data to be represented are obtained from soundings, and consist of sets of values of temperature, pressure, and humidity (e.g., relative humidity).
作者: 數(shù)量    時間: 2025-3-24 09:01

作者: 怒目而視    時間: 2025-3-24 12:25
https://doi.org/10.1007/978-1-4471-0039-3For instance, we may increase the temperature .. of a given mass of water to a temperature ..>.. by causing some paddles to rotate in the water, or by letting electrical current pass through a wire immersed in the water. In both cases external forces have performed a certain amount of work upon the system.
作者: BANAL    時間: 2025-3-24 15:26
Further Algebra and Applicationss process might actually occur at all. It is the second principle that faces this problem and provides at the same time a rigorous criterion to decide when a system is in a state of thermodynamic equilibrium.
作者: FEAT    時間: 2025-3-24 21:47

作者: Spinal-Fusion    時間: 2025-3-25 01:03

作者: 創(chuàng)作    時間: 2025-3-25 03:47
Further Adventures of The Dialectic of SexEvery portion of matter, the study of whose properties, interaction with other bodies, and evolution is undertaken from a thermodynamical point of view, is called a .. Once a system is defined, all the material environment with which it may eventually interact is called its ..
作者: 易受騙    時間: 2025-3-25 08:06

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作者: 和音    時間: 2025-3-25 23:51
Frédéric Bayart,Yanick Heurteauxake into account as another independent variable the total mass or the total number of moles, because this is assumed to be constant and, if we know the values of the extensive functions for the unit mass or the mole, generalization to any mass is done by simply multiplying by . or . (.: number of moles) (cf. Chapter I, Section 3).
作者: Leaven    時間: 2025-3-26 00:45

作者: Gratuitous    時間: 2025-3-26 07:04
glish to give the subject a specific and more extensive treatment. In writing the present textbook, we have tried to fill this rather remarkable gap in the literature related to atmospheric sciences. Our aim has been to provide students of meteorology with a book that can playa role similar to the t
作者: BOOM    時間: 2025-3-26 09:46
Vibrations with Two Degrees of Freedom,phere. By ‘vertical’ we mean that the atmosphere will be considered above a certain location on the Earth’s surface, generally taking into account neither the horizontal motions due to the Earth’s rotation and to horizontal gradients of pressure, nor the large-scale vertical motions.
作者: sorbitol    時間: 2025-3-26 12:40
Atmospheric Statics,phere. By ‘vertical’ we mean that the atmosphere will be considered above a certain location on the Earth’s surface, generally taking into account neither the horizontal motions due to the Earth’s rotation and to horizontal gradients of pressure, nor the large-scale vertical motions.
作者: originality    時間: 2025-3-26 19:25

作者: 極小量    時間: 2025-3-26 23:08
Book 1973dynamics of irreversible processes; on the other hand, consideration of heterogeneous and open homogeneous systems permits a rigorous formulation of the thermodynamic functions of clouds (exclusive of any consideration of microphysical effets) and a better understanding of the approx- imations usual
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作者: 琺瑯    時間: 2025-3-27 09:34
An Introduction to Automatic Control,e, while losing the same amount from the top (admittedly a gross over-simplification of actual radiative processes), lead to a steady distribution such as indicated by the dashed curve of Figure VIII-1. On the other hand, if we assume, in addition, a thorough vertical mixing, up to a level indicated
作者: 完全    時間: 2025-3-27 15:39
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作者: 儀式    時間: 2025-3-27 18:40
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