Quasi-biennial oscillation

Short description: Tropical wind alternation

The quasi-biennial oscillation (QBO) is a quasiperiodic oscillation of the equatorial zonal wind between easterlies and westerlies in the tropical stratosphere with a mean period of 28 to 29 months. The alternating wind regimes develop at the top of the lower stratosphere and propagate downwards at about 1 km (0.6 mi) per month until they are dissipated at the tropical tropopause. Downward motion of the easterlies is usually more irregular than that of the westerlies. The amplitude of the easterly phase is about twice as strong as that of the westerly phase. At the top of the vertical QBO domain, easterlies dominate, while at the bottom, westerlies are more likely to be found. At the 30mb level, with regards to monthly mean zonal winds, the strongest recorded easterly was 29.55 m/s in November 2005, while the strongest recorded westerly was only 15.62 m/s in June 1995.

## Contents

* 1 Theory
* 2 Effects
* 3 Observation of the QBO with weather balloons
* 4 Recent observations
* 5 See also
* 6 References
* 7 Further reading
* 8 External links

## Theory

In 1883, the eruption of Krakatoa led to visual tracking of subsequent volcanic ash in the stratosphere. This visual tracking led to the discovery of easterly winds between 25 and 30 km above the surface. The winds were then called the Krakatau easterlies. In 1908, data balloons launched above Lake Victoria in Africa recorded westerly winds in the stratospheric levels of the atmosphere. These findings, at the time, were thought to contradict the 1883 findings.[1] However, the winds that would become known as the QBO were discovered to oscillate between westerly and easterly in the 1950s by researchers at the UK Meteorological Office.[2] The cause of these QBO winds remained unclear for some time. Radiosonde soundings showed that its phase was not related to the annual cycle, as is the case for many other stratospheric circulation patterns. In the 1970s it was recognized by Richard Lindzen and James Holton that the periodic wind reversal was driven by atmospheric waves emanating from the tropical troposphere that travel upwards and are dissipated in the stratosphere by radiative cooling. The precise nature of the waves responsible for this effect was heavily debated; in recent years, however, gravity waves have come to be seen as a major contributor and the QBO is now simulated in a growing number of climate models.[3][4][5]

## Effects

Effects of the QBO include mixing of stratospheric ozone by the secondary circulation caused by the QBO, modification of monsoon precipitation, and an influence on stratospheric circulation in northern hemisphere winter (mediated partly by a change in the frequency of sudden stratospheric warmings). Easterly phases of the QBO often coincide with more sudden stratospheric warmings, a weaker Atlantic jet stream and cold winters in Northern Europe and eastern USA whereas westerly phases of the QBO often coincide with mild winters in eastern USA and a strong Atlantic jet stream with mild, wet stormy winters in northern Europe.[6] In addition, the QBO has been shown to affect hurricane frequency during hurricane seasons in the Atlantic.[7] Research has also been conducted investigating a possible relationship between ENSO (El Niño–Southern Oscillation) and the QBO.[8]

## Observation of the QBO with weather balloons

The Free University of Berlin supplies a QBO data set that comprises radiosonde observations from Canton Island, Gan, and Singapore. The plot below shows the QBO during the 1980s.

Time-height plot of monthly-mean, zonal-mean equatorial zonal wind (u) in m/s between about 20 and 35 km (22 mi) altitude above sea level over a ten-year period. Positive values denote westerly winds and the contour line is at 0 m/s.

## Recent observations

The first significant observed deviation from the normal QBO since its discovery in early 1950s was noted beginning in February 2016 when the transition to easterly winds was disrupted by a new band of westerly winds that formed unexpectedly. The lack of a reliable QBO cycle deprives forecasters of a valuable tool. Since the QBO has a strong influence on the North Atlantic Oscillation and thereby north European weather, scientists speculated that the coming winter could be warmer and stormier in that region.[9][10][11] NASA scientists have been researching to test if the extremely strong El Niño event of 2015/16, climate change, or some other factor might be involved. They are trying to determine if this is more of a once in a generation event, or if this is a sign of the changing climate.[12]

## See also

* North Atlantic oscillation

## References

1. ↑ Rohli, Robert V.; Vega, Anthony J. (2012). Climatology. p. 229. ISBN 9781449655914. https://books.google.com/books?id=WvuCyjEPxr4C&q=qbo+1800s&pg=PA229.
2. ↑ Graystone, P. (1959). "Meteorological office discussion on tropical meteorology". Met. Mag. 88: 117.
3. ↑ Takahashi, M. (1996). "Simulation of the stratospheric Quasi-Biennial Oscillation using a general circulation model". Geophys. Res. Lett. 23 (6): 661–4. doi:10.1029/95GL03413. Bibcode: 1996GeoRL..23..661T.
4. ↑ Scaife, A.A.; Butchart, N.; Warner, C.D.; Stainforth, D.; Norton, W.; Austin, J. (2000). "Realistic quasi-biennial oscillations in a simulation of the global climate". Geophys. Res. Lett. 27 (21): 3481–4. doi:10.1029/2000GL011625. Bibcode: 2000GeoRL..27.3481S.
5. ↑ Giorgetta, M.; Manzini, E.; Roeckner, E. (2002). "Forcing of the quasi-biennial oscillation from a broad spectrum of atmospheric waves". Geophys. Res. Lett. 29 (8): 861–4. doi:10.1029/2002GL014756. Bibcode: 2002GeoRL..29.1245G.
6. ↑ Ebdon, R.A. (1975). "The quasi-biennial oscillation and its association with tropospheric circulation patterns". Met. Mag. 104: 282–297.
7. ↑ Gray, William M. (1984). "Atlantic Seasonal Hurricane Frequency. Part I: El Nino and 30mb Quasi-Biennial Oscillation Influences". Monthly Weather Review 112 (9): 1649–1668. doi:10.1175/1520-0493(1984)112<1649:ashfpi>2.0.co;2. Bibcode: 1984MWRv..112.1649G.
8. ↑ Maruyama, T.; Tsuneoka, Y. (1988). "Anomalously short duration of the easterly wind phase of the QBO at 50hPa in 1987 and its relationship to an El Nino event". Journal of the Meteorological Society of Japan. Series II 66 (4): 629–634. doi:10.2151/jmsj1965.66.4_629.
9. ↑ Mason, Betsy (2016-09-07). "Unprecedented disruption to atmosphere's pacemaker foretells wet winter for Europe". Science. doi:10.1126/science.aah7277. https://www.science.org/content/article/unprecedented-disruption-atmospheres-pacemaker-foretells-wet-winter-europe. Retrieved 2016-09-09.
10. ↑ Newman, P. A.; Coy, L.; Pawson, S.; Lait, L. R. (28 August 2016). "The anomalous change in the QBO in 2015–2016". Geophys. Res. Lett. 43 (16): 8791–7. doi:10.1002/2016GL070373. Bibcode: 2016GeoRL..43.8791N. https://zenodo.org/record/1229062.
11. ↑ Osprey, Scott M.; Butchart, Neal; Knight, Jeff R.; Scaife, Adam A.; Hamilton, Kevin; Anstey, James A.; Schenzinger, Verena; Zhang, Chunxi (23 September 2016). "An unexpected disruption of the atmospheric quasi-biennial oscillation". Science 353 (6306): 1424–7. doi:10.1126/science.aah4156. PMID 27608666. Bibcode: 2016Sci...353.1424O. http://scholarspace.manoa.hawaii.edu/bitstream/10125/43740/1/Osprey et al..pdf.
12. ↑ Lynch, Patrick (2 September 2016), A Strange Thing Happened in the Stratosphere, https://www.nasa.gov/feature/goddard/2016/a-strange-thing-happened-in-the-stratosphere

## Further reading

* Andrews, David G.; Holton, James R.; Leovy, Conway B. (1987). Middle Atmosphere Dynamics. Academic Press. ISBN 978-0-12-058576-2. https://books.google.com/books?id=N1oNurYZefAC.
* Baldwin, M.P.; Gray, L.J.; Dunkerton, T.J.; Hamilton, K.; Haynes, P.H.; Randel, W.J.; Holton, J.R.; Alexander, M.J. et al. (2001). "The quasi‐biennial oscillation". Rev. Geophys. 39 (2): 179–229. doi:10.1029/1999RG000073. Bibcode: 2001RvGeo..39..179B.

## External links

* The Berlin QBO data series (1953–)
* NASA Goddard QBO web page (1980-present)

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