## Abstract In the present study, we have examined the influence of two major teleconnections, namely, El Niño Southern oscillation (ENSO) and Pacific decadal oscillation (PDO) on the summer monsoon precipitation of Myanmar. We used 52 years (1951–2002) of monthly precipitation data from a high‐res
Comparison of Stratospheric Zonal Winds and El Niño–Southern Oscillation in Recent Decades
✍ Scribed by R. P. Kane
- Publisher
- John Wiley and Sons
- Year
- 2004
- Tongue
- English
- Weight
- 159 KB
- Volume
- 24
- Category
- Article
- ISSN
- 0899-8418
- DOI
- 10.1002/joc.1004
No coin nor oath required. For personal study only.
✦ Synopsis
Abstract
A comparison of the plots of the monthly and yearly values indicates that stratospheric winds and El Niño–southern oscillation (ENSO) parameters evolve differently and probably have no relationship with each other. The sharp commencement of the 1997–98 El Niño in February–March 1997 was not accompanied by any particular deviation from the general trend of the wind variation in those months. Spectral analysis for 1979 up to the present indicates that winds have only a quasi‐biennial oscillation (QBO) near 2.40 years as a prominent variation, whereas ENSO has main periodicities near 3.7 and 5.0 years and a small QBO near 2.50 years, slightly but significantly different from the wind QBO. Copyright © 2004 Royal Meteorological Society
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