Periodic orbits and disturbance growth for baroclinic waves

Authors
Citation
Rm. Samelson, Periodic orbits and disturbance growth for baroclinic waves, J ATMOS SCI, 58(5), 2001, pp. 436-450
Citations number
26
Categorie Soggetti
Earth Sciences
Journal title
JOURNAL OF THE ATMOSPHERIC SCIENCES
ISSN journal
00224928 → ACNP
Volume
58
Issue
5
Year of publication
2001
Pages
436 - 450
Database
ISI
SICI code
0022-4928(2001)58:5<436:POADGF>2.0.ZU;2-M
Abstract
The growth of linear disturbances to stable and unstable time-periodic basi c states is analyzed in an asymptotic model of weakly nonlinear, baroclinic wave-mean interaction. In this model, an ordinary differential equation fo r the wave amplitude is coupled to a partial differential equation for the zonal-flow correction. Floquet vectors, the eigenmodes for linear disturban ces to the oscillatory basic states, split into wave-dynamical and decaying zonal-flow modes. Singular vectors reflect the structure of the Floquet ve ctors: the most rapid amplification and decay are associated with the wave- dynamical Floquet vectors, while the intermediate singular vectors closely follow the decaying zonal-flow Floquet vectors. Singular values depend stro ngly on initial and optimization times. For initial times near wave amplitu de maxima, the Floquet decomposition of the leading singular vector depends relatively weakly on optimization time. For the unstable oscillatory basic state in the chaotic regime, the leading Floquet vector is tangent to the large-scale structure of the attractor, while the leading singular vector i s not. However, corresponding inferences about the accessibility of disturb ed states rely on the simple attractor geometry, and may not easily general ize. The primary mechanism of disturbance growth on the wave timescale in t his model involves a time-dependent phase shift along the basic wave cycle. The Floquet vectors illustrate that modal disturbances to time-dependent b asic states can have time-dependent spatial structure, and that the latter need not indicate nonmodal dynamics. The dynamical splitting reduces the "b utterfly effect,'' the ability of small-scale disturbances to influence the evolution of an unstable large-scale flow.