Linear normal mode analysis of baroclinic instability in a meridional channel

Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2001.

Bibliographic Details
Main Author: Walker, Alison (Alison Elizabeth), 1971-
Other Authors: Joseph Pedlosky.
Format: Thesis
Language:eng
Published: Massachusetts Institute of Technology 2010
Subjects:
Online Access:http://hdl.handle.net/1721.1/57966
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author Walker, Alison (Alison Elizabeth), 1971-
author2 Joseph Pedlosky.
author_facet Joseph Pedlosky.
Walker, Alison (Alison Elizabeth), 1971-
author_sort Walker, Alison (Alison Elizabeth), 1971-
collection MIT
description Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2001.
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spelling mit-1721.1/579662019-04-13T00:06:51Z Linear normal mode analysis of baroclinic instability in a meridional channel Walker, Alison (Alison Elizabeth), 1971- Joseph Pedlosky. Massachusetts Institute of Technology. Dept. of Earth, Atmospheric, and Planetary Sciences. Massachusetts Institute of Technology. Dept. of Earth, Atmospheric, and Planetary Sciences. Earth, Atmospheric, and Planetary Sciences. Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2001. Includes bibliographical references (leaves 60-61). Numerical solutions of the unstable, growing modes are found for the two-layer inviscid quasigeostrophic equations in a meridional channel. A steady mean flow in the N-S direction is imposed in the upper layer, and it is assumed that changes in planetary vorticity following this mean flow are balanced by the input of vorticity from an imposed wind stress curl. Thus in the two-layer system, the vertical shear, in thermal wind balance, is associated with an interface slope which provides a gradient of potential vorticity (PV) in the x-direction, of equal magnitude and opposite sign in the two layers. In the y-direction the PV gradient has the value of planetary beta, [beta], in both layers. The unstable modes of this system exhibit a boundary-layer structure across the channel. They are intensified in the west. The growth rates of the unstable modes are of the same order as the zonal case, however the range of wavenumber and shear for which instability is possible is larger. Established cutoff criteria for the equal-layer zonal case are not applicable, and no analogous criteria has yet been found. Growing modes are found even for very weakly sheared flows, and this suggests that baroclinic instability may represent a more significant source of mid-ocean eddy energy than previously believed. by Alison Walker. S.M. 2010-09-01T13:34:41Z 2010-09-01T13:34:41Z 2001 2001 Thesis http://hdl.handle.net/1721.1/57966 49595962 eng M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission. http://dspace.mit.edu/handle/1721.1/7582 61 leaves application/pdf Massachusetts Institute of Technology
spellingShingle Earth, Atmospheric, and Planetary Sciences.
Walker, Alison (Alison Elizabeth), 1971-
Linear normal mode analysis of baroclinic instability in a meridional channel
title Linear normal mode analysis of baroclinic instability in a meridional channel
title_full Linear normal mode analysis of baroclinic instability in a meridional channel
title_fullStr Linear normal mode analysis of baroclinic instability in a meridional channel
title_full_unstemmed Linear normal mode analysis of baroclinic instability in a meridional channel
title_short Linear normal mode analysis of baroclinic instability in a meridional channel
title_sort linear normal mode analysis of baroclinic instability in a meridional channel
topic Earth, Atmospheric, and Planetary Sciences.
url http://hdl.handle.net/1721.1/57966
work_keys_str_mv AT walkeralisonalisonelizabeth1971 linearnormalmodeanalysisofbaroclinicinstabilityinameridionalchannel