The quasi-biennial oscillation

被引:1545
作者
Baldwin, MP
Gray, LJ
Dunkerton, TJ
Hamilton, K
Haynes, PH
Randel, WJ
Holton, JR
Alexander, MJ
Hirota, I
Horinouchi, T
Jones, DBA
Kinnersley, JS
Marquardt, C
Sato, K
Takahashi, M
机构
[1] NW Res Associates Inc, Bellevue, WA 98007 USA
[2] Rutherford Appleton Lab, Didcot OX11 0QX, Oxon, England
[3] Univ Hawaii, SOEST, Int Pacific Res Ctr, Honolulu, HI 96822 USA
[4] Univ Hawaii, Dept Meteorol, Honolulu, HI 96822 USA
[5] Univ Cambridge, Dept Appl Math & Theoret Phys, Ctr Atmospher Sci, Cambridge CB3 9EW, England
[6] Natl Ctr Atmospher Res, Div Atmospher Chem, Boulder, CO 80307 USA
[7] Univ Washington, Dept Atmospher Sci, Seattle, WA 98195 USA
[8] NW Res Associates Inc, Colorado Res Associates Div, Boulder, CO 80301 USA
[9] Kyoto Univ, Ctr Radio Atmospher Sci, Uji, Kyoto 6110011, Japan
[10] Kyoto Univ, Dept Geophys, Kyoto 6068502, Japan
[11] Harvard Univ, Div Engn & Appl Sci, Cambridge, MA 02138 USA
[12] Qwest, Seattle, WA USA
[13] Geoforschungszentrum Potsdam, D-14473 Potsdam, Germany
[14] Natl Inst Polar Res, Arctic Environm Res Ctr, Tokyo 1738515, Japan
[15] Univ Tokyo, Ctr Climate Syst Res, Meguro Ku, Tokyo 1538904, Japan
关键词
D O I
10.1029/1999RG000073
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The quasi-biennial oscillation (QBO) dominates the variability of the equatorial stratosphere (similar to 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 (similar to0-16 km) and mesosphere (similar to 50-100 km). It is intended to provide a broad overview of the QBO and its effects to researchers outside the held, 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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页码:179 / 229
页数:51
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