Universal dependences between turbulent and mean flow parameters instably and neutrally stratified Planetary Boundary Layers

We consider the resistance law for the planetary boundary layer (PBL) from the point of view of the similarity theory. In other words, we select the set of the PBL governing parameters and search for an optimal way to express through these parameters the geostrophic drag coefficient <i>C<su...

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Main Authors: I. N. Esau, S. S. Zilitinkevich
Format: Article
Language:English
Published: Copernicus Publications 2006-01-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/13/135/2006/npg-13-135-2006.pdf
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spelling doaj-492172b444ac48f28f0d5408e0a62a482020-11-24T22:58:14ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462006-01-01132135144Universal dependences between turbulent and mean flow parameters instably and neutrally stratified Planetary Boundary LayersI. N. EsauI. N. EsauS. S. ZilitinkevichS. S. ZilitinkevichS. S. ZilitinkevichWe consider the resistance law for the planetary boundary layer (PBL) from the point of view of the similarity theory. In other words, we select the set of the PBL governing parameters and search for an optimal way to express through these parameters the geostrophic drag coefficient <i>C<sub>g</sub>=u<sub>*</sub> /U<sub>g</sub></i> and the cross isobaric angle &alpha; (where <i>u<sub>*</sub></i> is the friction velocity and <i>U<sub>g</sub></i> is the geostrophic wind speed). By this example, we demonstrate how to determine the 'parameter space' in the most convenient way, so that make independent the dimensionless numbers representing co-ordinates in the parameter space, and to avoid (or at least minimise) artificial self-correlations caused by the appearance of the same factors (such as <i>u<sub>*</sub></i>) in the examined dimensionless combinations (e.g. in <i>C<sub>g</sub>=u<sub>*</sub> /U<sub>g</sub></i>) and in dimensionless numbers composed of the governing parameters. We also discuss the 'completeness' of the parameter space from the point of view of large-eddy simulation (LES) modeller creating a database for a specific physical problem. As recognised recently, very large scatter of data in prior empirical dependencies of <i>C<sub>g</sub></i> and &alpha; on the surface Rossby number Ro=<i>U<sub>g</sub>| fz<sub>0</sub>|<sup>-1</sup></i> (where <i>z<sub>0</sub></i> is the roughness length) and the stratification characterised by &micro; was to a large extent caused by incompactness of the set of the governing parameters. The most important parameter overlooked in the traditional approach is the typical value of the Brunt-Väisälä frequency <i>N</i> in the free atmosphere (immediately above the PBL), which involves, besides Ro and &micro;, one more dimensionless number: &micro;<i><sub>N</sub>=N/ | f |</i>. Accordingly, we consider <i>C<sub>g</sub></i> and &alpha; as dependent on the three (rather then two) basic dimensionless numbers (including &micro;<sub><i>N</i></sub>) using LES database DATABASE64. By these means we determine the form of the dependencies under consideration in the part of the parameter space representing typical atmospheric PBLs, and provide analytical expressions for <i>C<sub>g</sub></i> and &alpha;.http://www.nonlin-processes-geophys.net/13/135/2006/npg-13-135-2006.pdf
collection DOAJ
language English
format Article
sources DOAJ
author I. N. Esau
I. N. Esau
S. S. Zilitinkevich
S. S. Zilitinkevich
S. S. Zilitinkevich
spellingShingle I. N. Esau
I. N. Esau
S. S. Zilitinkevich
S. S. Zilitinkevich
S. S. Zilitinkevich
Universal dependences between turbulent and mean flow parameters instably and neutrally stratified Planetary Boundary Layers
Nonlinear Processes in Geophysics
author_facet I. N. Esau
I. N. Esau
S. S. Zilitinkevich
S. S. Zilitinkevich
S. S. Zilitinkevich
author_sort I. N. Esau
title Universal dependences between turbulent and mean flow parameters instably and neutrally stratified Planetary Boundary Layers
title_short Universal dependences between turbulent and mean flow parameters instably and neutrally stratified Planetary Boundary Layers
title_full Universal dependences between turbulent and mean flow parameters instably and neutrally stratified Planetary Boundary Layers
title_fullStr Universal dependences between turbulent and mean flow parameters instably and neutrally stratified Planetary Boundary Layers
title_full_unstemmed Universal dependences between turbulent and mean flow parameters instably and neutrally stratified Planetary Boundary Layers
title_sort universal dependences between turbulent and mean flow parameters instably and neutrally stratified planetary boundary layers
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 2006-01-01
description We consider the resistance law for the planetary boundary layer (PBL) from the point of view of the similarity theory. In other words, we select the set of the PBL governing parameters and search for an optimal way to express through these parameters the geostrophic drag coefficient <i>C<sub>g</sub>=u<sub>*</sub> /U<sub>g</sub></i> and the cross isobaric angle &alpha; (where <i>u<sub>*</sub></i> is the friction velocity and <i>U<sub>g</sub></i> is the geostrophic wind speed). By this example, we demonstrate how to determine the 'parameter space' in the most convenient way, so that make independent the dimensionless numbers representing co-ordinates in the parameter space, and to avoid (or at least minimise) artificial self-correlations caused by the appearance of the same factors (such as <i>u<sub>*</sub></i>) in the examined dimensionless combinations (e.g. in <i>C<sub>g</sub>=u<sub>*</sub> /U<sub>g</sub></i>) and in dimensionless numbers composed of the governing parameters. We also discuss the 'completeness' of the parameter space from the point of view of large-eddy simulation (LES) modeller creating a database for a specific physical problem. As recognised recently, very large scatter of data in prior empirical dependencies of <i>C<sub>g</sub></i> and &alpha; on the surface Rossby number Ro=<i>U<sub>g</sub>| fz<sub>0</sub>|<sup>-1</sup></i> (where <i>z<sub>0</sub></i> is the roughness length) and the stratification characterised by &micro; was to a large extent caused by incompactness of the set of the governing parameters. The most important parameter overlooked in the traditional approach is the typical value of the Brunt-Väisälä frequency <i>N</i> in the free atmosphere (immediately above the PBL), which involves, besides Ro and &micro;, one more dimensionless number: &micro;<i><sub>N</sub>=N/ | f |</i>. Accordingly, we consider <i>C<sub>g</sub></i> and &alpha; as dependent on the three (rather then two) basic dimensionless numbers (including &micro;<sub><i>N</i></sub>) using LES database DATABASE64. By these means we determine the form of the dependencies under consideration in the part of the parameter space representing typical atmospheric PBLs, and provide analytical expressions for <i>C<sub>g</sub></i> and &alpha;.
url http://www.nonlin-processes-geophys.net/13/135/2006/npg-13-135-2006.pdf
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