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THE DIURNAL VARIATION OF THE ABSOLUTE HUMIDITY IN THE ATMOSPHERE SURFACE BOUNDARY LAYER,
AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
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The first section of this paper contains an analysis of experimental data obtained during special observations at the Koltushi station during the summers of 1957 and 1958. The second contains a theoretical solution of the problem of the diurnal variation of humidity, using the equation of eddy diffusion of water vapor. The eddy coefficient is assumed to be both height- and time-dependent. An example is given of the calculation of the diurnal variation of humidity, and the computational and experimental results are compared. Author
APPROVED FOR PUBLIC RELEASE