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A revised method of presenting wavenumber–frequency power spectrum diagrams that reveals the asymmetric nature of tropical large-scale waves
Author(s) -
Winston C. Chao,
Bo Yang,
Xiouhua Fu
Publication year - 2008
Publication title -
climate dynamics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.026
H-Index - 163
eISSN - 1432-0894
pISSN - 0930-7575
DOI - 10.1007/s00382-008-0494-3
Subject(s) - rossby wave , physics , kelvin wave , wavenumber , gravity wave , geophysics , equatorial waves , gravitational wave , scale (ratio) , infragravity wave , spectral density , computational physics , mechanical wave , mechanics , geology , wave propagation , meteorology , longitudinal wave , astrophysics , atmospheric sciences , optics , computer science , telecommunications , quantum mechanics , latitude , astronomy , equator
The popular method of presenting wavenumber–frequency power spectrum diagrams for studying tropical large-scale waves in the literature is shown to give an incomplete presentation of these waves. The so-called “convectively coupled Kelvin (mixed Rossby-gravity) waves” are presented as existing only in the symmetric (anti-symmetric) component of the diagrams. This is obviously not consistent with the published composite/regression studies of “convectively coupled Kelvin waves,” which illustrate the asymmetric nature of these waves. The cause of this inconsistency is revealed in this note and a revised method of presenting the power spectrum diagrams is proposed. When this revised method is used, “convectively coupled Kelvin waves” show anti-symmetric components, and “convectively coupled mixed Rossby-gravity waves (also known as Yanai waves)” show a hint of symmetric components. These results bolster a published proposal that these waves should be called “chimeric Kelvin waves,” “chimeric mixed Rossby-gravity waves,” etc. This revised method of presenting power spectrum diagrams offers an additional means of comparing the GCM output with observations by calling attention to the capability of GCMs to correctly simulate the asymmetric characteristics of equatorial waves.

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