Investigation of the Upper Layers of the Atmosphere and Space
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Publisher :
Page : 69 pages
File Size : 21,70 MB
Release : 1964
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ISBN :
Author :
Publisher :
Page : 69 pages
File Size : 21,70 MB
Release : 1964
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ISBN :
Author :
Publisher :
Page : 80 pages
File Size : 36,45 MB
Release : 1964
Category : Astronautics in meteorology
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Author : I. A. Khvostikov
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Page : 836 pages
File Size : 10,20 MB
Release : 1965
Category : Atmosphere, Upper
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Author : Ivan Andreevich Khvostikov
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Page : 604 pages
File Size : 47,11 MB
Release : 1965
Category : Upper atmosphere
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Author : John Clifford Bird
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Page : 40 pages
File Size : 23,76 MB
Release : 1988
Category : Atmosphere, Upper
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Author : A. A. Blagonravov
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Page : 53 pages
File Size : 28,77 MB
Release : 1964
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Author : A. A. Blagonravov
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Page : 1 pages
File Size : 11,82 MB
Release : 1964
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ISBN :
This is a report on USSR space research with scientific satellites, rocket probes, and radioastronomy. The report includes a discussion on intrumentation and findings of several types of research satellites. It discusses the findings of a series of explorer rockets probes and radiolocation of the planets Mercury, Venus and Mars.
Author : Hugh Odishaw
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Page : 616 pages
File Size : 27,52 MB
Release : 1964
Category : Geophysics
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Author :
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Page : 40 pages
File Size : 41,36 MB
Release : 1989
Category : Atmosphere, Upper
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Author : PLUMB
Publisher : Birkhäuser
Page : 465 pages
File Size : 40,43 MB
Release : 2013-11-21
Category : Science
ISBN : 3034858256
PAGEOPH, stratosphere, these differences provide us with new evidence, interpretation of which can materially help to advance our understanding of stratospheric dynamics in general. It is now weil established that smaller-scale motions-in particular gravity waves and turbulence-are of fundamental importance in the general circulation of the mesosphere; they seem to be similarly, if less spectacularly, significant in the troposphere, and probably also in the stratosphere. Our understanding of these motions, their effects on the mean circulation and their mutual interactions is progressing rapidly, as is weil illustrated by the papers in this issue; there are reports of observational studies, especially with new instruments such as the Japanese MV radar, reviews of the state of theory, a laboratory study and an analysis of gravity waves and their effects in the high resolution "SKYHI" general circulation model. There are good reasons to suspect that gravity waves may be of crucial significance in making the stratospheric circulation the way it is (modeling experience being one suggestive piece of evidence for this). Direct observational proof has thus far been prevented by the difficulty of making observations of such scales of motion in this region; in one study reported here, falling sphere observations are used to obtain information on the structure and intensity of waves in the upper stratosphere.