## Abstract The plausible long‐term trend of precipitation in China and its association with El Niño–southern oscillation (ENSO) are investigated by using non‐parametric techniques. It is concluded that a greater number of decreasing trends are observed than are expected to occur by chance. Geograp
El Niño and its effect on precipitation in Arizona and Western New Mexico
✍ Scribed by Andrade, Edward R. ;Sellers, William D.
- Book ID
- 102390807
- Publisher
- Wiley (John Wiley & Sons)
- Year
- 1988
- Weight
- 499 KB
- Volume
- 8
- Category
- Article
- ISSN
- 2314-6214
No coin nor oath required. For personal study only.
✦ Synopsis
This paper focuses primarily on the effect of El Niiio on seasonal and annual precipitation at 26 locations in Arizona and western New Mexico for an 86-year period from 1900 to 1985. Following Rasmusson (1984), each year is classified as either a non-El Niiio year (51) or an El Niiio year (33, with the El Niiios designated as being very weak (4), weak (8), moderate (12), or strong (1 1). Using the Mann-Whitney U-test for the 19 stations in Arizona, we find that, in the spring (March-May) and in the autumn (September-November), there is a positive relationship between precipitation in Arizona and both moderate and strong El Niiios.
These results are verified by correlating seasonal and annual precipitation for the complete 26-station network with the pressure difference between Tahiti and Darwin. Plausible physical explanations for these results are given.
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