4.6 Article

Evidence for short vertical wavelength Kelvin waves in the Department of Energy-Atmospheric Radiation Measurement Nauru99 radiosonde data

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
Volume 106, Issue D17, Pages 20125-20129

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2001JD900108

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Stratospheric zonal wind and temperature oscillations observed in a 30 day time series of four times per day radiosonde data taken as part of Nauru99 show a strong negative quadrature relationship at periods of 9.5 days and 5 days. The 9.5-day waves have vertical wavelength of about 4.5 km, and are deduced to be Kelvin waves of zonal wave number 2; the 5-day waves have vertical wavelengths in the range of 3-4.5 km, and are deduced to be Kelvin waves of zonal wavenumber 4. Vertical momentum fluxes associated with the 9.5- and 5-day modes are estimated to be 1 x 10(-4) m(2)s(-2) and 2 x 10(-4) m(2)s(-2), respectively, in the 20-25 km altitude range where the mean zonal flow is characteristic of the westerly phase of the quasi-biennial oscillation (QBO). These are an order of magnitude smaller than momentum fluxes associated with traditional wavenumber 1 Kelvin waves analyzed in the easterly phase of the QBO.

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