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

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朦胧

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Purpose of the Symposiumand applications.” A wealth of scientific experience has proven that such exchanges inspire new findings, generate new concepts, and refresh and stimulate the seekers of new knowledge and those who apply such knowledge in the service of society.

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Book 1968tions, and the advancement of its professional ideals." The organization of the Society took place in affiliation with the American Association for the Advancement of Science at Saint Louis, Missouri, December 29, 1919, and its incorporation, at Washington, D. C., January 21, 1920. The work of the S

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Lower Atmospheric Energy Sources for the Upper Atmospherees and thermal and gravitational tides, and the factors influencing their transmission to the upper atmosphere are discussed. In the case of tides a quantitative description of the magnitudes and energetics is presented. A simple model for evaluating the thermal effects of wave dissipation is also presented.

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The Influence of the Neutral Wind Field on the Distribution of Ionization in the E-Region shown to be responsible for the production of two layers in a recent experiment. It is suggested that this neutral convergence mechanism may be responsible for the low-altitude layers whose occurrence cannot be predicted by the mechanisms depending solely on vertical shear of the horizontal neutral wind.