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A model of the quasi‐biennial oscillation on an equatorial beta‐plane

Plumb, R. Alan, Bell, Robert C.·1982·Quarterly Journal of the Royal Meteorological Society

Abstract

An equatorial beta‐plane model of equatorial wave‐mean flow interaction in the lower stratosphere is described. Kelvin and mixed Rossby‐gravity waves generated by a specified forcing on the lower boundary radiate upward through the model domain where they are subject to thermal and mechanical dissipation. The wave‐mean flow feedback problem is solved on the assumption that changes in the zonal mean state occur slowly enough for the wave field to be steady, locally in time. A quasi‐biennial oscillation develops in the model with a period of about 1000 days. A novel feature of this model is the incorporation of latitudinal structure and of thermal and meridional wind components of the oscillation. The influence of the meridional circulation on the structure of the zonal wind oscillation is discussed in some detail.

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Metadata

Authors
Plumb, R. A., & Bell, R. C.
Venue
Quarterly Journal of the Royal Meteorological Society
Publisher
Wiley
Published
1982-04
Volume
108
Issue
456
Pages
335-352
ISSN
  • 0035-9009 (ISSN-L)
  • 1477-870X
OpenAlex
W2168707266
Cited by
342
References
0
FWCI
5.86
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: A model of the quasi‐biennial oscillation on an equatorial beta‐plane. https://app.cochat.ai/papers/10.1002/qj.49710845604
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Plumb, R. A., & Bell, R. C. (1982). A model of the quasi‐biennial oscillation on an equatorial beta‐plane. Quarterly Journal of the Royal Meteorological Society. https://doi.org/10.1002/qj.49710845604

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.