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contributor authorGoodman, Jason C.
contributor authorMarshall, John
date accessioned2017-06-09T14:37:59Z
date available2017-06-09T14:37:59Z
date copyright2002/11/01
date issued2002
identifier issn0022-4928
identifier otherams-23209.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159745
description abstractThe authors explore the use of the ?neutral vectors? of a linearized version of a global quasigeostrophic atmospheric model with realistic mean flow in the study of the nonlinear model's low-frequency variability. Neutral vectors are the (right) singular vectors of the linearized model's tendency matrix that have the smallest eigenvalues; they are also the patterns that exhibit the largest response to forcing perturbations in the linear model. A striking similarity is found between neutral vectors and the dominant patterns of variability (EOFs) observed in both the full nonlinear model and in the real world. The authors discuss the physical and mathematical connection between neutral vectors and EOFs. Investigation of the ?optimal forcing patterns??the left singular vectors?proves to be less fruitful. The neutral modes have equivalent barotropic vertical structure, but their optimal forcing patterns are baroclinic and seem to be associated with low-level heating. But the horizontal patterns of the forcing patterns are not robust and are sensitive to the form of the inner product used in the singular vector decomposition analysis. Additionally, applying ?optimal? forcing patterns as perturbations to the full nonlinear model does not generate the response suggested by the linear model.
publisherAmerican Meteorological Society
titleUsing Neutral Singular Vectors to Study Low-Frequency Atmospheric Variability
typeJournal Paper
journal volume59
journal issue22
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(2002)059<3206:UNSVTS>2.0.CO;2
journal fristpage3206
journal lastpage3222
treeJournal of the Atmospheric Sciences:;2002:;Volume( 059 ):;issue: 022
contenttypeFulltext


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