Decay of the El Niño with Different Intensity. Part II, Decay of the Moderate and Relatively-Weak El Niño

In Part II, we explored the decay processes of the moderate and relatively‐weak El Niño. The results show that for the moderate El Niño, the anomalous signals appear in the development and peak phase, then they decay quickly after the peak phase due to the insufficient intensity of the El Niño. This...

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Published in:Chinese journal of geophysics 2010-11, Vol.53 (6), p.915-925
Main Authors: Chang‐Zheng, LIU, Feng, XUE
Format: Article
Language:English
Subjects:
Advective mode
Decay
Moderate El Niño
Relatively-weak El Niño
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description In Part II, we explored the decay processes of the moderate and relatively‐weak El Niño. The results show that for the moderate El Niño, the anomalous signals appear in the development and peak phase, then they decay quickly after the peak phase due to the insufficient intensity of the El Niño. This is similar to the abortion of the western Pacific oscillation process. For this reason, different from the strong El Niño, the moderate El Niño turns into a normal state. For the relatively‐weak El Niño, its phase transition is controlled by another mechanism. With the enhancement and westward movement of the subtropical high over the southeastern Pacific, the easterly and sea surface temperature anomalies also extend westward from the tropical eastern Pacific. The above process is an advective mode that causes the relatively‐weak El Niño turning into a La Niña.
doi_str_mv 10.1002/cjg2.1562
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source Alma/SFX Local Collection
subjects Advective mode
Decay
Moderate El Niño
Relatively-weak El Niño
title Decay of the El Niño with Different Intensity. Part II, Decay of the Moderate and Relatively-Weak El Niño
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