Titlebook: Meteorological Investigations of the Upper Atmosphere; R. S. Quiroz Book 1968 American Meteorological Society 1968 Mesosphere.Ionosphere.T

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书目名称Meteorological Investigations of the Upper Atmosphere影响因子(影响力)




书目名称Meteorological Investigations of the Upper Atmosphere影响因子(影响力)学科排名




书目名称Meteorological Investigations of the Upper Atmosphere网络公开度




书目名称Meteorological Investigations of the Upper Atmosphere网络公开度学科排名




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Research on the Lower Fringe of Spaceeen the motions of the neutral atmosphere and the ionized portion; interactions, both by dynamic processes and by radiative transfer, between the upper and lower atmosphere; and refinement of indirect probing techniques which can be used to study this region from the ground or from satellites. Recen

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Aerospace Systems Requirements for Environmental Data in the Altitude Range 60–200 Kmthe 60–200 km layer of the atmosphere. If history repeats itself, some urgently needed atmospheric data may not be recognized at the present stage of development of these vehicles any more than was the need for information on clear air turbulence data foreseen 10–15 years ago by designers and operat

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Lower Atmospheric Energy Sources for the Upper Atmosphere conversion. Brief attention is devoted to energy reaching the upper atmosphere by radiation and diffusion. Energy carried to the upper atmosphere by advection by the mean field and by vertically propagating waves is treated in greater detail. The explicit excitations of gravity waves, planetary wav

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Composition of the Mesosphere and Lower Thermosphere of the major constituents of the atmosphere. Above the turbopause, diffusive separation exists and the composition rapidly changes with increasing altitude. In the atmosphere the change probably does not occur sharply and the transition may be spread over an altitude range of as much as 30 km. For

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Temperature, Density and Pressure Variations in the Stratosphere and the Mesosphereriability of temperature, density and pressure in the stratosphere and mesosphere from 25 to 55 km. The results, which are in general agreement with those of previous investigations, show large changes with season at high latitudes, with the greatest variability in winter and spring. Standard deviat

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