Forcing mechanism of the seasonally asymmetric quasi‐biennial oscillation secondary circulation in ERA‐40 and MAECHAM5

Abstract

The seasonality of the quasi‐biennial oscillation (QBO) and its secondary circulation is analyzed in the European Reanalysis (ERA‐40) and Middle Atmosphere European Centre Hamburg Model (MAECHAM5) general circulation model data sets through the multitaper method‐singular value decomposition (MTM‐SVD). In agreement with previous studies, the results reveal a strong seasonal dependence of the QBO secondary circulation. This is characterized by a two‐cell structure symmetric about the equator during autumn and spring. However, anomalies strongly weaken in the summer hemisphere and strengthen in the winter hemisphere, leading to an asymmetric QBO secondary circulation characterized by a single‐cell structure displaced into the winter hemisphere during the solstices. In ERA‐40, this asymmetry is more pronounced during the northern than during the southern winter. These results provide the first observation of the QBO secondary circulation asymmetries in the ERA‐40 reanalysis data set across the full stratosphere and the lower mesosphere, up to 0.1 hPa. The MTM‐SVD reconstruction of the seasonal QBO signals in the residual circulation and the QBO signals in Eliassen Palm (EP) flux divergences suggest a particular mechanism for the seasonal asymmetries of the QBO secondary circulation and its extension across the midlatitudes. The analysis shows that the QBO modulates the EP flux in the winter hemispheric surf zone poleward of the QBO jets. The zonal wind forcing by EP flux divergence is transformed by the Coriolis effect into a meridional wind signal. The seasonality in the stratospheric EP flux and the hemispheric differences in planetary wave forcing cause the observed seasonality in the QBO secondary circulation and its hemispheric differences.