The DOI matches its Crossref record; 96 of the 96 references it cites were found in a registry or an index.
The quasi‐biennial oscillation
Open accessAbstract
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.
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Citations
Cites
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Application of the cross wavelet transform and wavelet coherence to geophysical time series
Grinsted, A., Moore, J. C., & Jevrejeva, S. (2004) · Nonlinear Processes in Geophysics · doi:10.5194/npg-11-561-2004 · Cited by 6,285
Atmospheric and Oceanic Fluid Dynamics: Fundamentals and Large-Scale Circulation
Vallis, G. K. (2017) · doi:10.1017/9781107588417 · Cited by 1,891
Stratospheric aerosol-Observations, processes, and impact on climate
Kremser, S., Thomason, L. W., von Hobe, M., Hermann, M., Deshler, T., Timmreck, C., Toohey, M., Stenke, A., Schwarz, J. P., Weigel, R., et al. (2016) · Reviews of Geophysics · doi:10.1002/2015rg000511 · Cited by 578
Technical Note: The CCCma third generation AGCM and its extension into the middle atmosphere
Scinocca, J. F., McFarlane, N. A., Lazare, M., Li, J., & Plummer, D. (2008) · Atmospheric Chemistry and Physics · doi:10.5194/acp-8-7055-2008 · Cited by 459
Lawrence, Z. D., Perlwitz, J., Butler, A. H., Manney, G. L., Newman, P. A., Lee, S. H., & Nash, E. R. (2020) · Journal of Geophysical Research: Atmospheres · doi:10.1029/2020jd033271 · Cited by 313
Metadata
- Authors
- Baldwin, M. P., Gray, L. J., Dunkerton, T. J., Hamilton, K., Haynes, P. H., Randel, W. J., Holton, J. R., Alexander, M. J., Hirota, I., Horinouchi, T., Jones, D. B. A., Kinnersley, J. S., Marquardt, C., Sato, K., & Takahashi, M.
- Venue
- Reviews of Geophysics
- Publisher
- American Geophysical Union (AGU)
- Published
- 2001-05
- Volume
- 39
- Issue
- 2
- Pages
- 179-229
- ISSN
- 0096-1043 (ISSN-L)
- 8755-1209
- 1944-9208
- OpenAlex
- W2025415734
- Cited by
- 2,113
- References
- 96
- FWCI
- 29.78
- Type
- journal article
- Language
- en
- Open access
- bronze
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- Baldwin, M. P., Gray, L. J., Dunkerton, T. J., Hamilton, K., Haynes, P. H., Randel, W. J., Holton, J. R., Alexander, M. J., Hirota, I., Horinouchi, T., Jones, D. B. A., Kinnersley, J. S., Marquardt, C., Sato, K., & Takahashi, M. (2001). The quasi‐biennial oscillation. Reviews of Geophysics. https://doi.org/10.1029/1999rg000073
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