Parameterization of meandering phenomenon in a stable atmospheric boundary layer

被引:1
|
作者
da Costa Carvalho, Jonas
Degrazia, Gervasio Annes [1 ]
Tulio de Vilhena, Marco
Magalhaes, Sergio Garcia
Goulart, Antonio G.
Anfossi, Domenico
Acevedo, Otavio Costa
Moraes, Osvaldo L. L.
机构
[1] Univ Fed Santa Maria, Dept Fis, BR-97119900 Santa Maria, RS, Brazil
[2] Univ Luterana Brasil, Canoas, Brazil
[3] Univ Fed Rio Grande do Sul, Inst Matemat, Porto Alegre, RS, Brazil
[4] Univ Reg Integrada, Dept Ciencias Exatas, Santo Angelo, Brazil
[5] CNR, Ist Sci Atmosfera & Clima, I-10126 Turin, Italy
关键词
meandering parameterization; Lagrangian stochastic particle model; meandering enhanced diffusion of passive scalars; stable atmospheric boundary layer;
D O I
10.1016/j.physa.2005.11.060
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
Accounting for the current knowledge of the stable atmospheric boundary layer (ABL) turbulence structure and characteristics, a new formulation for the meandering parameters to be used in a Lagrangian stochastic particle turbulent diffusion model has been derived. That is, expressions for the parameters controlling the meandering oscillation frequency in low wind speed stable conditions are proposed. The classical expression for the meandering autocorrelation function, the turbulent statistical diffusion theory and ABL similarity theory are employed to estimate these parameters. In addition, this new parameterization was introduced into a particular Lagrangian stochastic particle model, which is called Iterative Langevin solution for low wind, validated with the data of Idaho National Laboratory experiments, and compared with others diffusion models. The results of this new approach are shown to agree with the measurements of Idaho experiments and also with those of the other atmospheric diffusion models. The major advance shown in this study is the formulation of the meandering parameters expressed in terms of the characteristic scales (velocity and length scales) describing the physical structure of a turbulent stable boundary layer. These similarity formulas can be used to simulate meandering enhanced diffusion of passive scalars in a low wind speed stable ABL. (c) 2006 Elsevier B.V. All rights reserved.
引用
收藏
页码:247 / 256
页数:10
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