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contributor authorReinhold, Brian
date accessioned2017-06-09T14:26:32Z
date available2017-06-09T14:26:32Z
date copyright1986/07/01
date issued1986
identifier issn0022-4928
identifier otherams-19317.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155420
description abstractThe linear evolution of arbitrarily specified perturbations in a zonally homogeneous, two-layer model is analyzed in a dynamical system which describes the disturbances in terms of the phase difference and amplitude ratio between the temperature and streamfunction components. The stationary equilibria of this system are equivalent to the individual eigenmodes of normal mode analysis and in the inviscid case, simple analytical expressions for these equilibria are possible. These expressions allow us to quantitatively examine the physical processes that determine the normal mode structures in the inviscid case and how the processes of friction then affect them. The advantage to this approach is that a conceptual understanding for the processes determining the so-called ?preferred structure? and their characteristics (e.g., growth rates) of normal mode analysis is obtained in terms of the basic Quid flow properties of advection, dispersion and dissipation. But the most important conceptual property we find is that in the presence of dissipation the normal modes are indeed ?preferred structure? or deterministic, in the sense that any arbitrarily specified initial perturbation evolves asymptotically to that structure. This is not always the case in the inviscid problem or certain cases of symmetrically applied dissipation. However, the occurrence of determinism in this simple case allows us to conceptually investigate and understand the equilibrated truncated nonlinear state in terms of the linear solution.
publisherAmerican Meteorological Society
titleStructural Determinism of Linear Baroclinic Waves and Simple Nonlinear Equilibration
typeJournal Paper
journal volume43
journal issue14
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1986)043<1484:SDOLBW>2.0.CO;2
journal fristpage1484
journal lastpage1504
treeJournal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 014
contenttypeFulltext


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