On the tidal interaction of a solar-type star with an orbiting companion: Excitation of g mode oscillation and orbital evolution

(1998)

Authors:

C Terquem, JCB Papaloizou, RP Nelson, DNC Lin

A comparison of empirical orthogonal decomposition methods in baroclinic flows

Dynamics of Atmospheres and Oceans 27:1-4 (1998) 649-660

Authors:

AV Stephen, IM Moroz, PL Read, WG Früh

Abstract:

The relative merits of three contrasting empirical orthogonal decomposition methods in common use (namely, Proper Orthogonal Decomposition, Biorthogonal Decomposition and Multivariate Singular Systems Analysis) are considered as applied to baroclinic flow data. The regimes analysed are a steady, drifting wave, a modulated amplitude vacillating wave flow and a neighbouring multi-mode state which exhibits intermittency. The results are used to make a qualitative comparison of the methods in terms of convergence properties, variance capture and eigenfunction structure. The feasibility of using the resulting empirical orthogonal functions to transform partial differential equations to ordinary differential equations by Galerkin projection is mentioned. © 1997 Elsevier Science B.V.

Wave interactions and baroclinic chaos: A paradigm for long timescale variability in planetary atmospheres

CHAOS SOLITON FRACT 9:1-2 (1998) 231-249

Authors:

PL Read, M Collins, WG Fruh, SR Lewis, AF Lovegrove

Abstract:

Baroclinic instability is the principal mode of non-axisymmetric flow in the large-scale atmospheric circulation at mid-latitudes, and is responsible for oganising the structure and behaviour of major weather systems. This instability can also be fruitfully studied in the laboratory under controlled conditions. In this paper, we review recent work carried out by the authors and collaborators on various routes to chaotic behaviour in rotating, stratified flows. Results include the discovery of new multi-mode regimes in which small ensembles of baroclinic waves interact in a nonlinear mode competition with the thermally-driven axisymmetric component of the Bow, generating chaotic oscillatory variability on very long timescales. We discuss various attempts to capture this type of behaviour in simple models, and consider the significance of the phenomenon as a paradigm for understanding the nature of long timescale variability in the climates of the Earth and Mars. (C) 1998 Elsevier Science Ltd. All rights reserved.

Experiments on the structure of baroclinic waves and zonal jets in an internally heated, rotating, cylinder of fluid

PHYSICS OF FLUIDS 10:2 (1998) 374-389

Authors:

ME Bastin, PL Read

On the Global Warping of a Thin Self-gravitating Near-Keplerian Gaseous Disk with Application to the Disk in NGC 4258

The Astrophysical Journal 497 (1998) 212-226

Authors:

JCB Papaloizou, C Terquem, DNC Lin