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On the horizontal and vertical variability of the vertical turbulent eddy diffusion coefficients in the mesosphere

Author: S P Zimmerman; T J Keneshea; U.S. Air Force Geophysics Laboratory. Aeronomy Division.
Publisher: Hanscom AFB, Mass. : Aeronomy Division, Air Force Geophysics Laboratory, Air Force Systems Command, USAF, [1983]
Series: AFGL-TR, 83-227.; Environmental research papers (Hanscom AFB, Mass.), no. 851.
Edition/Format:   Print book : National government publication : EnglishView all editions and formats
Database:WorldCat
Summary:
Utilizing the premise of turbulent energy balance and an altitude-invariant non-dimensional relations of turbulent heat flux, vertical turbulent diffusivities are obtained from bodies of data consisting of winds and temperature in the upper atmosphere. These are specific to the small scale turbulent motions of the atmosphere and should be differentiated from those determined from the study of wave interactive  Read more...
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Details

Material Type: Government publication, National government publication
Document Type: Book
All Authors / Contributors: S P Zimmerman; T J Keneshea; U.S. Air Force Geophysics Laboratory. Aeronomy Division.
OCLC Number: 10873670
Notes: Cover title.
Distributed to depository libraries in microfiche.
"22 August 1983."
Description: 16 pages : illustrations ; 28 cm.
Series Title: AFGL-TR, 83-227.; Environmental research papers (Hanscom AFB, Mass.), no. 851.
Responsibility: S.P. Zimmerman, T.J. Keneshea.

Abstract:

Utilizing the premise of turbulent energy balance and an altitude-invariant non-dimensional relations of turbulent heat flux, vertical turbulent diffusivities are obtained from bodies of data consisting of winds and temperature in the upper atmosphere. These are specific to the small scale turbulent motions of the atmosphere and should be differentiated from those determined from the study of wave interactive damping mechanisms. The average values of the turbulent diffusivities derived in this work are presented as a function of latitude, and are compared to those derived by an alternative method.

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