## 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
Correlation between El Niño–Southern Oscillation (ENSO) and precipitation in South-east Asia and the Pacific region
✍ Scribed by Z. X. Xu; K. Takeuchi; H. Ishidaira
- Publisher
- John Wiley and Sons
- Year
- 2004
- Tongue
- English
- Weight
- 193 KB
- Volume
- 18
- Category
- Article
- ISSN
- 0885-6087
- DOI
- 10.1002/hyp.1315
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✦ Synopsis
Abstract
The relationship between El Niño–Southern Oscillation (ENSO) events versus precipitation anomalies, and the response of seasonal precipitation to El Niño and La Niña events were investigated for 30 basins that represent a range of climatic types throughout South‐east Asia and the Pacific region. The teleconnection between ENSO and the hydroclimate is tested using both parametric and non‐parametric approaches, and the lag correlations between precipitation anomalies versus the Southern Oscillation Index (SOI) several months earlier, as well as the coherence between SOI and precipitation anomalies are estimated. The analysis shows that dry conditions tend to be associated with El Niño in the southern zone, and part of the middle zone in the study area. The link between precipitation anomalies and ENSO is statistically significant in the southern zone and part of the middle zone of the study area, but significant correlation was not observed in the northern zone. Patterns of precipitation response may differ widely among basins, and even the response of a given river basin to individual ENSO events also may be changeable. Copyright © 2003 John Wiley & Sons, Ltd.
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## Abstract Snowmelt runoff dominates streamflow in the Upper Rio Grande (URG) basin of New Mexico and Colorado. Annual variations in streamflow timing and volume at most stations in the region are strongly influenced by the El Niño–southern oscillation (ENSO) through its modulation of the seasonal