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contributor authorPauluis, Olivier
date accessioned2017-06-09T16:34:37Z
date available2017-06-09T16:34:37Z
date copyright2011/01/01
date issued2010
identifier issn0022-4928
identifier otherams-70299.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4212064
description abstractThe impact of water vapor on the production of kinetic energy in the atmosphere is discussed here by comparing two idealized heat engines: the Carnot cycle and the steam cycle. A steam cycle transports water from a warm moist source to a colder dryer sink. It acts as a heat engine in which the energy source is the latent heat of evaporation. It is shown here that the amount of work produced by a steam cycle depends on relative humidity and is always less than that produced by the corresponding Carnot cycle. The Carnot and steam cycles can be combined into a mixed cycle that is forced by both sensible and latent heating at the warm source. The work performed depends on four parameters: the total energy transport; the temperature difference between the energy source and sink; the Bowen ratio, which measures the partitioning between the sensible and latent heat transports; and the relative humidity of the atmosphere. The role of relative humidity on the work produced by a steam cycle is discussed in terms of the Gibbs free energy and in terms of the internal entropy production.
publisherAmerican Meteorological Society
titleWater Vapor and Mechanical Work: A Comparison of Carnot and Steam Cycles
typeJournal Paper
journal volume68
journal issue1
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/2010JAS3530.1
journal fristpage91
journal lastpage102
treeJournal of the Atmospheric Sciences:;2010:;Volume( 068 ):;issue: 001
contenttypeFulltext


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