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Reexamining the Indian Summer Monsoon Rainfall–ENSO Relationship From Its Recovery in the 21 st Century: Role of the Indian Ocean SST Anomaly Associated With Types of ENSO Evolution
Author(s) -
Yu ShiYun,
Fan Lei,
Zhang Yu,
Zheng XiaoTong,
Li Ziguang
Publication year - 2021
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2021gl092873
Subject(s) - el niño southern oscillation , anomaly (physics) , climatology , sea surface temperature , monsoon , indian ocean , environmental science , southern oscillation , multivariate enso index , atmospheric sciences , geology , oceanography , physics , condensed matter physics
This study found that the relationship between the Indian Summer Monsoon Rainfall (ISMR) and El Niño‐Southern Oscillation (ENSO) has recovered since 2001, and the relationship strength is closely related to the summer tropical Indian Ocean (TIO) sea surface temperature (SST) anomaly, with the TIO warming (cooling) indicating a stronger (weaker) relationship. Under the same El Niño/La Niña scenario, different signs of the TIO anomaly indicate distinct atmospheric circulation anomalies over the Indian Ocean, thus affecting the ISMR–ENSO relationship. The TIO anomaly is principally associated with different types of ENSO temporal evolution. Strong El Niño events with an early onset, and the transition of El Niño to La Niña, tend to have a warmer TIO and a stronger ISMR–ENSO relationship, in contrast to most of the cases of a decaying La Niña or a La Niña that persists throughout the year. The result brings a prospect for improving the ISMR prediction.