Abstract
Using 25 years of National Meteorological Center (NMC) data for 1964-88 the relation between tropical and extratropical quasi-biennial oscillations (QBOs) was examined for zonally averaged quantities and planetary-wave Eliassen-Palm fluxes in the Northern Hemisphere winter. The extratropical QBO discussed by Holton and Tan existed in both temporal halves of the dataset. Autocorrelation analysis demonstrated that it was an important mode of interannual variability in the extratropical winter stratosphere. Correlation with the tropics was strongest when 40-mb equatorial winds were used to define the tropical QBO. Easterly phase at 40 mb implied a weaker than normal polar night jet and warmer than normal polar temperature and vice versa. An opposite relationship was obtained using 10-mb equatorial winds. -from Authors
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CITATION STYLE
Dunkerton, T. J., & Baldwin, M. P. (1991). Quasi-biennial modulation of planetary-wave fluxes in the Northern Hemisphere winter. Journal of the Atmospheric Sciences, 48(8), 1043–1061. https://doi.org/10.1175/1520-0469(1991)048<1043:QBMOPW>2.0.CO;2
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