Abstract
This study revisits the relations between Madden-Julian Oscillation (MJO) and El Niño that is classified as eastern Pacific (EP) and central Pacific (CP) types. During an EP-type event that produces lasting dry conditions in the Maritime Continent and western Pacific, the MJO activity is weak especially in its 4th-6th phases as a strong response. In contrast during CP-type episodes, the MJO exhibits notably enhanced and suppressed amplitudes in its different phases. The low-level westerly wind anomalies of enhanced MJO impact the CP-type El Niño more than vice versa.
| Original language | English |
|---|---|
| Pages (from-to) | 32-37 |
| Number of pages | 6 |
| Journal | Atmospheric Science Letters |
| Volume | 16 |
| Issue number | 1 |
| DOIs | |
| State | Published - Jan 1 2015 |
Keywords
- CP El Niño
- EP El Niño
- MJO
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