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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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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
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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
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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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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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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.
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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.
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