Japan Geoscience Union Meeting 2025

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS06] Atmospheric (Stratosphere-troposphere) Processes And their Role in Climate

Tue. May 27, 2025 10:45 AM - 12:15 PM 105 (International Conference Hall, Makuhari Messe)

convener:Shunsuke Noguchi(Department of Earth and Planetary Sciences, Faculty of Science, Kyushu University), Yayoi Harada(Meteorological Research Institute), Kazuaki Nishii(Graduate School of Bioresources, Mie University), Nawo Eguchi(Research Institute for Applied Mechanics, Kyushu University), Chairperson:Kazuaki Nishii(Graduate School of Bioresources, Mie University), Nawo Eguchi(Research Institute for Applied Mechanics, Kyushu University)



12:00 PM - 12:15 PM

[AAS06-11] Revisiting the cross-equatorial symmetry in QBO jets

*Takatoshi Sakazaki1, Kevin Hamilton2 (1.Graduate School of Science, Kyoto University, 2.University of Hawai'i)

Keywords:Quasi-Biennial Oscillation, reanalysis

The stratospheric Quasi-Biennial Oscillation (QBO) is usually defined by the interannual variability in the deseasonalized zonal-mean zonal wind in the equatorial stratosphere. As shown by many studies, the long-term average QBO jets take their maximum right on the equator with their meridional structure being symmetric with respect to the equator. By using multiple reanalysis datasets, the present study demonstrates that the meridional structure systematically depends on the QBO phase and month. Specifically, in either phase of QBO (westerly or easterly), the QBO jets tend to sit in the winter hemisphere. Such seasonal dependence is likely due to the meridional transport of zonal momentum by cross-equatorial flow associated with the seasonally-varying Brewer-Dobson circulation. The meridional asymmetry may need to be considered when reconstructing a single QBO index time series by synthesizing zonal wind data at different locations (e.g., FUB wind).