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Reconstructing the vertical profile of humidity on the basis of the vertical profile of temperatureThe vertical profile of humidity in the atmosphere is developed on the basis of the vertical profile of temperature using an empirical formula linking changes in humidity with changes in temperature and altitude. The atmosphere is divided into three layers by altitude, since the condition for the formation of humidity varies with altitude.
Document ID
19750005378
Acquisition Source
Legacy CDMS
Document Type
Other
Authors
Bazlova, T. I. (Linguistic Systems, Inc. Cambridge, MA, United States)
Date Acquired
August 8, 2013
Publication Date
November 1, 1974
Publication Information
Publication: Automation of the Collection and Analysis of Sci. Inform. in the Probl. of the Interaction of the Atmosphere and Ocean (NASA-TT-F-801)
Subject Category
Geophysics
Accession Number
75N13450
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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