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A novel index for depicting Enso transition with application in Enso-East Asian summer monsoon relationship

Bibliographic Data

ID15549690
AuthorsJiaxin Chen (0009-0002-7669-5016, Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), corresponding author), Song Yang (0000-0002-6712-3991, Key Laboratory of Guangdong Province), Xianghui Fang (0000-0002-1210-0055, Fudan University), Shuheng Lin (0000-0001-8951-7417, Fujian Normal University), Jhayron S Pérez‐Carrasquilla (0000-0001-9672-8490, University of Maryland, College Park), Fenying Cai (0009-0004-0572-4179, Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)), Weizhen Chen (0000-0002-1660-9537, Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)), Jia Wu (0000-0002-7421-7275, Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou))
Year2024
Volume19
Issue12
Pages124066-124066
Publication date2024-11-14
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ad9290
OpenAlexW4404368223
LanguageEN
References cited81

The impact of El Niño-Southern Oscillation (ENSO) transition on the East Asian summer monsoon (EASM) during post-ENSO summer has been investigated widely, but how to quantify ENSO transition precisely is still a challenge. This study proposes a new index to quantify ENSO transition based on the intensity of the spring persistence barrier. After validation through the key processes that influence ENSO transition, the index could be further validated by investigating the relationship between transitive/persistent ENSO events and the EASM. For the transitive ENSO events, the cold sea surface temperature (SST) anomaly in the central Pacific during post-ENSO summer strengthens the anticyclone over the western Pacific and the EASM by reinforcing the Walker circulation and the local Hadley circulation. In contrast, during the persistent ENSO events, the prolonged warm SST anomaly in the central Pacific exerts a relatively weaker impact on the EASM due to a less robust atmospheric response over the western Pacific

Climatology · East Asia · East Asian Monsoon · El Niño Southern Oscillation · Geography · Index (typography · La Niña · Monsoon · Multivariate ENSO index · Climate variability and models · Computer Science · Environmental Science · Meteorological Phenomena and Simulations · Solar Radiation and Photovoltaics · Geology

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