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Modeling of turbulent transport in the surface layerThe turbulence equations as written by Donaldson using the method of invariant modeling have been applied to the following limiting cases of the surface or constant flux layer of the planetary boundary layer: (1) Neutrally stable; (2) stable (above influence of surface roughness); (3) nearly neutrally stable; and (4) very unstable (free convection). For the neutrally stable case, the equations are shown to admit as a solution the familiar logarithmic profile. By use of this result, boundary conditions suitable for the surface layer are defined and are simple to apply to rough surfaces.
Document ID
19740004043
Acquisition Source
Legacy CDMS
Document Type
Other - NASA Technical Note (TN)
Authors
Smith, G. L.
(NASA Langley Research Center Hampton, VA, United States)
Date Acquired
September 3, 2013
Publication Date
December 1, 1973
Subject Category
Geophysics
Report/Patent Number
L-8917
NASA-TN-D-7306
Accession Number
74N12156
Funding Number(s)
PROJECT: RTOP 160-44-63-04
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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