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Equatorial waves in the lower stratosphere. I: A novel detection method

Tindall, J. C., Thuburn, J. and Highwood, E. J. (2006) Equatorial waves in the lower stratosphere. I: A novel detection method. Quarterly Journal of the Royal Meteorological Society, 132 (614). pp. 177-194. ISSN 1477-870X

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Abstract/Summary

Wavenumber-frequency spectral analysis and linear wave theory are combined in a novel method to quantitatively estimate equatorial wave activity in the tropical lower stratosphere. The method requires temperature and velocity observations that are regularly spaced in latitude, longitude and time; it is therefore applied to the ECMWF 15-year re-analysis dataset (ERA-15). Signals consistent with idealized Kelvin and Rossby-gravity waves are found at wavenumbers and frequencies in agreement with previous studies. When averaged over 1981-93, the Kelvin wave explains approximately 1 K-2 of temperature variance on the equator at 100 hPa, while the Rossby-gravity wave explains approximately 1 m(2)s(-2) of meridional wind variance. Some inertio-gravity wave and equatorial Rossby wave signals are also found; however the resolution of ERA-15 is not sufficient for the method to provide an accurate climatology of waves with high meridional structure.

Item Type:Article
Divisions:Faculty of Science > School of Mathematical and Physical Sciences > Department of Meteorology
ID Code:5400
Uncontrolled Keywords:inertio-gravity wave Kelvin wave Rossby-gravity wave QUASI-BIENNIAL OSCILLATION MERIDIONAL WIND OSCILLATIONS INERTIA-GRAVITY WAVES KELVIN WAVES TROPICAL STRATOSPHERE OBSERVATIONAL EVIDENCE FREQUENCY DOMAIN CONVECTION MOMENTUM FLUCTUATIONS
Additional Information:Part A
Publisher:Royal Meteorological Society

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