The maintenance of low-frequency atmospheric anomalies
A linear diagnostic analysis of four prominent low-frequency atmospheric perturbation patterns in a GCM is carried out to determine the mechanism responsible for the maintenance of these patterns. Results indicate that interactions between the low-frequency patterns and the time-mean zonal asymmetries of the model climate are crucial to the maintenance of the patterns. Of equal importance are anomalous fluxes from transients. Vorticity fluxes due to bandpass (1-7 days) fluctuations ranging over broad sectors of the globe were found to be the most important components of the maintenance of flux anomalies. The nonlinear interactions of the low-frequency deviations with themselves were only of secondary importance.