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SAE Technical Paper Series, 1962
<div class="htmlview paragraph">This study of the characteristics of the upper atmosphere are directed primarily toward determining their effects on space vehicles. Methods of calculating density, pressure, and temperature, and also the variations of these values caused by diurnal, seasonal, and solar influences, are discussed in relation to ...
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<div class="htmlview paragraph">This study of the characteristics of the upper atmosphere are directed primarily toward determining their effects on space vehicles. Methods of calculating density, pressure, and temperature, and also the variations of these values caused by diurnal, seasonal, and solar influences, are discussed in relation to ...
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The structure of the Uranus atmosphere
Icarus, 1980Abstract A series of radiative/connvective models is presented for the Uranus atmosphere for various methane-to-hydrogen mixing ratios and internal heat fluxes. The variation of flux through the atmosphere, which is largely defined by absorption of sunlight in methane bands, the partial pressure of methane, which is taken to be limited by saturated ...
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ON THE STRUCTURE OF ATMOSPHERIC VORTICES
Journal of Meteorology, 1951Abstract Several features of atmospheric vortices (symmetric tropical cyclones) are examined kinematically by use of the vorticity and circulation theorems. First, generation of a region of negative relative vorticity around a tropical cyclone is derived from the vorticity theorem, and then its necessity is shown from the divergence of integrals of the
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Structure and Optics of the Atmosphere
1966Among the latest achievements of science has been an increased understanding of the earth’s atmosphere — its structure and the processes operating within it. Still far from complete, these concepts have been worked out just in the past quarter century (see, for example, [175]). Scientists of the elder generation well recall the time when the atmosphere
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Aerostatics: Structure of the Atmosphere
1934As noted in I1 an ideal fluid is conceived of as composed of small elements or particles having mass and moving freely and without shearing stress, one relative to another. We must also assume the existence of a gravity field as a result of which the pressure at any point in the fluid is measured by the action of gravity on the particles lying between ...
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