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

Warming Early Mars with Carbon Dioxide Clouds That Scatter Infrared Radiation

Science American Association for the Advancement of Science (AAAS) 278:5341 (1997) 1273-1276

Authors:

François Forget, Raymond T Pierrehumbert

Lower-Tropospheric Heat Transport in the Pacific Storm Track

Journal of the Atmospheric Sciences American Meteorological Society 54:11 (1997) 1533-1543

Authors:

Kyle L Swanson, Raymond T Pierrehumbert

A GCM climate database for Mars: For mission planning and for scientific studies

ADV SPACE RES 19:8 (1997) 1213-1222

Authors:

PL Read, M Collins, F Forget, R Fournier, F Hourdin, SR Lewis, O Talagrand, FW Taylor, NPJ Thomas

Abstract:

The construction of a new database of statistics on the climate and environment of the Martian atmosphere is currently under way, with the support of the European Space Agency. The primary objectives of this database are to provide information for mission design specialists on the mean state and variability of the Martian environment in unprecedented detail, through the execution of a set of carefully validated simulations of the Martian atmospheric circulation using comprehensive numerical general circulation models. The formulation of the models used are outlined herein, noting especially new improvements in various schemes to parametrize important physical processes, and the scope of the database to be constructed is described. A novel approach towards the representation of large-scale variability in the output of the database using empirical eigenfunctions derived from statistical analyses of the numerical simulations, is also discussed. It is hoped that the resulting database will be of value for both scientific and engineering studies of Mars' atmosphere and near-surface environment. (C) 1997 COSPAR. Published by Elsevier Science Ltd.