2.1
Hemispheric modes, regimes and forced change (INVITED)
John C. Fyfe, Canadian Centre for Climate Modelling and Analysis, Victoria, BC, Canada
The leading mode of hemispheric sea level pressure (SLP) is referred to as the Arctic Oscillation (AO) in the case of Northern Hemisphere SLP and the Antarctic Oscillation (AAO) in the case of Southern Hemisphere SLP. These modes are very influential in terms of the many climatic variables with which they co-vary (and in some instances drive) and very expansive in terms of their spatial extent. It is also known that the time-series characterizing the temporal behavior of these modes exhibit significant linear trends, which modelling studies suggest may be the consequence of enhanced greenhouse gas forcing.
We begin our presentation with a brief description and comparison of these leading modes of hemispheric variability with an emphasis on their respective roles in polar climate variability and change. Following this we address the important issue of whether or not these modes are in fact the best description of hemispheric variability and change. The AO and AAO are usually obtained using linear principal component analysis which produces the optimal, although somewhat restrictive, linear approximation to the data. In an attempt to overcome this limitation we apply the recently introduced nonlinear principal component analysis which finds the optimal nonlinear approximation to the data. It is shown for example that Northern Hemispheric SLP variability is best characterized by three distinct quasi-stationary states, to which the AO is the best linear compromise. One of the regimes, for example, is reminiscent of the negative phase of the North Atlantic Oscillation which the analysis shows displays a substantial downward trend in its frequency of occupation. Interestingly, this observed downward trend can be reproduced with a global climate model subject to enhanced greenhouse gas forcing. We conclude the presentation by characterizing the leading Northern and Southern Hemisphere nonlinear regimes of variability with an emphasis on their respective roles in polar climate variability and change.
Session 2, Large-scale Atmospheric Circulations, Oscillations, and Interactions
Tuesday, 15 May 2001, 8:30 AM-10:00 AM
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