An Objective Method for Determining the Generalized Transport Tensor for Two-Dimensional Eulerian ModelsSource: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 007::page 1319Author:Danielsen, Edwin F.
DOI: 10.1175/1520-0469(1981)038<1319:AOMFDT>2.0.CO;2Publisher: American Meteorological Society
Abstract: An objective method for deriving the components of a generalized transport tensor for a two-dimensional model is presented. The method uses representative meridional and vertical velocities and thermodynamic scalars at a uniform grid to reduce the problem to solving two flux equations for two unknowns. One unknown is the streamfunction, coefficient of an antisymmetric tensor, which corrects the Eulerian mean motions for Stokes drift. The other is a time constant, which converts the deviatory velocity tensor (Reynold's stress tensor for temporal averaging) to a symmetric transport tensor. The complete asymmetric tensor is called a transport rather than a diffusion tensor because its divergence yields both advection and diffusion by the deviatory velocities. Advantages and disadvantages of Lagrangian and Eulerian averages are also discussed.
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contributor author | Danielsen, Edwin F. | |
date accessioned | 2017-06-09T14:22:20Z | |
date available | 2017-06-09T14:22:20Z | |
date copyright | 1981/07/01 | |
date issued | 1981 | |
identifier issn | 0022-4928 | |
identifier other | ams-18152.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4154126 | |
description abstract | An objective method for deriving the components of a generalized transport tensor for a two-dimensional model is presented. The method uses representative meridional and vertical velocities and thermodynamic scalars at a uniform grid to reduce the problem to solving two flux equations for two unknowns. One unknown is the streamfunction, coefficient of an antisymmetric tensor, which corrects the Eulerian mean motions for Stokes drift. The other is a time constant, which converts the deviatory velocity tensor (Reynold's stress tensor for temporal averaging) to a symmetric transport tensor. The complete asymmetric tensor is called a transport rather than a diffusion tensor because its divergence yields both advection and diffusion by the deviatory velocities. Advantages and disadvantages of Lagrangian and Eulerian averages are also discussed. | |
publisher | American Meteorological Society | |
title | An Objective Method for Determining the Generalized Transport Tensor for Two-Dimensional Eulerian Models | |
type | Journal Paper | |
journal volume | 38 | |
journal issue | 7 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1981)038<1319:AOMFDT>2.0.CO;2 | |
journal fristpage | 1319 | |
journal lastpage | 1339 | |
tree | Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 007 | |
contenttype | Fulltext |