The quasi‐biennial oscillation
Top Cited Papers
Open Access
- 1 May 2001
- journal article
- Published by American Geophysical Union (AGU) in Reviews of Geophysics
- Vol. 39 (2) , 179-229
- https://doi.org/10.1029/1999rg000073
Abstract
The quasi‐biennial oscillation (QBO) dominates the variability of the equatorial stratosphere (∼16–50 km) and is easily seen as downward propagating easterly and westerly wind regimes, with a variable period averaging approximately 28 months. From a fluid dynamical perspective, the QBO is a fascinating example of a coherent, oscillating mean flow that is driven by propagating waves with periods unrelated to that of the resulting oscillation. Although the QBO is a tropical phenomenon, it affects the stratospheric flow from pole to pole by modulating the effects of extratropical waves. Indeed, study of the QBO is inseparable from the study of atmospheric wave motions that drive it and are modulated by it. The QBO affects variability in the mesosphere near 85 km by selectively filtering waves that propagate upward through the equatorial stratosphere, and may also affect the strength of Atlantic hurricanes. The effects of the QBO are not confined to atmospheric dynamics. Chemical constituents, such as ozone, water vapor, and methane, are affected by circulation changes induced by the QBO. There are also substantial QBO signals in many of the shorter‐lived chemical constituents. Through modulation of extratropical wave propagation, the QBO has an effect on the breakdown of the wintertime stratospheric polar vortices and the severity of high‐latitude ozone depletion. The polar vortex in the stratosphere affects surface weather patterns, providing a mechanism for the QBO to have an effect at the Earth's surface. As more data sources (e.g., wind and temperature measurements from both ground‐based systems and satellites) become available, the effects of the QBO can be more precisely assessed. This review covers the current state of knowledge of the tropical QBO, its extratropical dynamical effects, chemical constituent transport, and effects of the QBO in the troposphere (∼0–16 km) and mesosphere (∼50–100 km). It is intended to provide a broad overview of the QBO and its effects to researchers outside the field, as well as a source of information and references for specialists. The history of research on the QBO is discussed only briefly, and the reader is referred to several historical review papers. The basic theory of the QBO is summarized, and tutorial references are provided.Keywords
This publication has 247 references indexed in Scilit:
- Simulation of the Quasi‐Biennial Oscillation in a general circulation modelGeophysical Research Letters, 1999
- Quasi‐biennial modulation of the southern hemisphere stratospheric polar vortexGeophysical Research Letters, 1998
- The first simulation of an ozone QBO in a general circulation modelGeophysical Research Letters, 1998
- Effects of the quasi‐biennial oscillation on the zonally averaged transport of tracersJournal of Geophysical Research: Atmospheres, 1998
- Mixing zone in the tropical stratosphere above 10 mbGeophysical Research Letters, 1996
- Long‐term variability in the equatorial middle atmosphere zonal windJournal of Geophysical Research: Atmospheres, 1996
- Gravity wave activity associated with tropical convection detected in TOGA COARE Sounding dataGeophysical Research Letters, 1996
- Stratosphere‐troposphere exchangeReviews of Geophysics, 1995
- Gravity wave activity in the lower atmosphere: Seasonal and latitudinal variationsJournal of Geophysical Research: Atmospheres, 1995
- On the interannual variability of trace gases in the middle atmosphereGeophysical Research Letters, 1990