Search from over 60,000 research works

Advanced Search

Nonlinear stability of Eady's model

[thumbnail of 1520-0469(1994)051_3427_nsoem_2.0.co;2.pdf]
Preview
1520-0469(1994)051_3427_nsoem_2.0.co;2.pdf - Published Version (612kB) | Preview
Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Mu, M. and Shepherd, T. G. orcid id iconORCID: https://orcid.org/0000-0002-6631-9968 (1994) Nonlinear stability of Eady's model. Journal of the Atmospheric Sciences, 51 (23). pp. 3427-3436. ISSN 1520-0469 doi: 10.1175/1520-0469(1994)051<3427:NSOEM>2.0.CO;2

Abstract/Summary

A nonlinear stability theorem is established for Eady's model of baroclinic flow. In particular, the Eady basic state is shown to be nonlinearly stable (for arbitrary shear) provided (Δz)/(Δy) > 2(5)^1/2f/(πN),where Δz is the height of the domain, Δy the channel width, f the Coriolis parameter, and N the buoyancy frequency. When this criterion is satisfied, explicit bounds can be derived on the disturbance potential enstrophy, the disturbance energy, and the disturbance available potential energy on the rigid lids, which are expressed in terms of the initial disturbance fields. The disturbances are completely general (with nonzero potential vorticity) and are not assumed to be of small amplitude. The results may be regarded as an extension of Arnol'd's second nonlinear stability theorem to continuously stratified quasigeostrophic baroclinic flow.

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/32897
Item Type Article
Refereed Yes
Divisions No Reading authors. Back catalogue items
Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Publisher American Meteorological Society
Download/View statistics View download statistics for this item

Downloads

Downloads per month over past year

University Staff: Request a correction | Centaur Editors: Update this record

Search Google Scholar