Unveiling the role of South Tropical Atlantic in winter Atlantic Niño inducing La Niña

The boreal winter-peaked Atlantic Niño/Niña can influence La Niña/El Niño (the cold/warm phase of El Niño-Southern Oscillation, ENSO) in the following year. However, the Atlantic Niño-La Niña relationship is more uncertain than the Atlantic Niña-El Niño counterpart. Here, we show that this uncertainty arises from two distinct types of Atlantic Niño events: the Equatorial and Expanded types, which differ in their meridional sea surface temperature (SST) warming. The Equatorial type, with SST warming confined to the equator, has a weaker climate impact due to limited influence on local convective heating in spring when the intertropical convergence zone (ITCZ) shifts southward. In contrast, the Expanded type, with SST warming extending into the southern tropical Atlantic (STA), drive persistent local anomalous convection heating and strong remote atmospheric responses in the tropical Pacific from winter to spring. Our results emphasize the critical role of STA conditions in shaping the influence of winter Atlantic Niño on the Pacific.

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Publication Details

Journal
Nature Communications
Published
2025-02-13
DOI
https://doi.org/10.1038/s41467-025-56874-y
Citations
7
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
7.74

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article

Unveiling the role of South Tropical Atlantic in winter Atlantic Niño inducing La Niña

Hanjie Fan, Jiepeng Chen, Xin Wang, Lei Zhang et al.
7 citations
Nature Communications
Climate variability and models
7.74
article

Unveiling the role of South Tropical Atlantic in winter Atlantic Niño inducing La Niña

Hanjie Fan, Jiepeng Chen, Xin Wang, Lei Zhang, Dongxiao Wang, Mengyan Chen, Guangli Zhang
article en
7 citations

Abstract

The boreal winter-peaked Atlantic Niño/Niña can influence La Niña/El Niño (the cold/warm phase of El Niño-Southern Oscillation, ENSO) in the following year. However, the Atlantic Niño-La Niña relationship is more uncertain than the Atlantic Niña-El Niño counterpart. Here, we show that this uncertainty arises from two distinct types of Atlantic Niño events: the Equatorial and Expanded types, which differ in their meridional sea surface temperature (SST) warming. The Equatorial type, with SST warming confined to the equator, has a weaker climate impact due to limited influence on local convective heating in spring when the intertropical convergence zone (ITCZ) shifts southward. In contrast, the Expanded type, with SST warming extending into the southern tropical Atlantic (STA), drive persistent local anomalous convection heating and strong remote atmospheric responses in the tropical Pacific from winter to spring. Our results emphasize the critical role of STA conditions in shaping the influence of winter Atlantic Niño on the Pacific.

Nature CommunicationsVol. 16(1)
Sun Yat-sen University (CN), Institute of Oceanology (CN), South China Sea Institute Of Oceanology (CN), Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) (CN), Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) (CN)
National Natural Science Foundation of China, Chinese Academy of Sciences, China Postdoctoral Science Foundation, Natural Science Foundation of Guangdong Province, Youth Innovation Promotion Association of the Chinese Academy of Sciences, South China Sea Institute of Oceanology, Chinese Academy of Sciences, National Key Research and Development Program of China, Youth Innovation Promotion Association, Basic and Applied Basic Research Foundation of Guangdong Province
Life below water
Openalex Percentile: Top 3%
Climate variability and models
7.74
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