On the source of midlatitude low-frequency variability. Part I: a statistical approach to persistence

Abstract

The forcing of low-frequency variability by synoptic transient traveling perturbations is investigated within a quasi-geostrophic channel forced by a localized baroclinic jet. Spontaneously generated baroclinic perturbations grow and decay along a storm track; at the end of the track a maximum of low-frequency variability is obtained, in agreement with atmospheric observations. The structure of low-frequency variability is studied with a combination of statistical methods, using a multivariate red noise model as a random reference. We show that the anomalies are preferentialy linked with local stationary structures or long-wave vacillations according to their location and their sign. The transient feedback has a positive role in extending the jet downstream but the primary effect is the maintenance of the block circulation. -from Authors