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Titlebook: Atmospheric Thermodynamics; J. V. Iribarne,W. L. Godson Book 1973 Springer Science+Business Media Dordrecht 1973 thermodynamics

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發(fā)表于 2025-3-21 16:22:20 | 只看該作者 |倒序瀏覽 |閱讀模式
期刊全稱Atmospheric Thermodynamics
影響因子2023J. V. Iribarne,W. L. Godson
視頻videohttp://file.papertrans.cn/165/164649/164649.mp4
圖書封面Titlebook: Atmospheric Thermodynamics;  J. V. Iribarne,W. L. Godson Book 1973 Springer Science+Business Media Dordrecht 1973 thermodynamics
影響因子The thermodynamics of the atmosphere is the subject of several chapters in most textbooks on dynamic meteorology, but there is no work in English 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 textbooks on chemical thermodynamics for the chemists. This implies a previous knowledge of general thermodynamics, such as students acquire in general physics courses; therefore, although the basic principles are reviewed (in the first four chapters), they are only briefly discussed, and emphasis is laid on those topics that will be useful in later chapters, through their application to atmospheric problems. No attempt has been made to introduce the thermodynamics 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
Pindex Book 1973
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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.
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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
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發(fā)表于 2025-3-22 06:14:52 | 只看該作者
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).
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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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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).
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