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contributor authorDanielsen, Edwin F.
date accessioned2017-06-09T14:22:20Z
date available2017-06-09T14:22:20Z
date copyright1981/07/01
date issued1981
identifier issn0022-4928
identifier otherams-18152.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154126
description abstractAn 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.
publisherAmerican Meteorological Society
titleAn Objective Method for Determining the Generalized Transport Tensor for Two-Dimensional Eulerian Models
typeJournal Paper
journal volume38
journal issue7
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1981)038<1319:AOMFDT>2.0.CO;2
journal fristpage1319
journal lastpage1339
treeJournal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 007
contenttypeFulltext


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