Asymmetric ENSO Forcing on the South Pacific Meridional Mode

Abstract The South Pacific Meridional Mode (SPMM) influences El Niño‐Southern Oscillation (ENSO) variability, but whether ENSO triggers SPMM remains unclear. We show that ENSO can induce an in‐phase SPMM event via atmospheric teleconnections, beginning in early boreal summer of the ENSO‐developing y...

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Main Authors: Cheng Qi, Fan Jia
Format: Article
Language:English
Published: Wiley 2025-07-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2025GL117165
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author Cheng Qi
Fan Jia
author_facet Cheng Qi
Fan Jia
author_sort Cheng Qi
collection DOAJ
description Abstract The South Pacific Meridional Mode (SPMM) influences El Niño‐Southern Oscillation (ENSO) variability, but whether ENSO triggers SPMM remains unclear. We show that ENSO can induce an in‐phase SPMM event via atmospheric teleconnections, beginning in early boreal summer of the ENSO‐developing year, with a negative asymmetry. Strong La Niña induces negative SPMM more effectively than El Niño induces positive SPMM, due to differences in ENSO teleconnections and their intensity. During boreal summer and fall of strong La Niña, intense transient eddy feedback reshapes the Pacific‐South America pattern into a South Pacific Oscillation‐like pressure dipole, strengthening trade winds and promoting negative SPMM growth, a process absent in El Niño. In boreal winter, stronger La Niña teleconnections sustain negative SPMM into spring. Half of the negative SPMM events co‐occur with negative North Pacific Meridional Mode, contributing to multi‐year La Niña development. These findings advance the understanding of SPMM and its impact on ENSO.
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spelling doaj-art-92a08a8f3e3a4f05be9b502f76f10a132025-07-26T08:35:57ZengWileyGeophysical Research Letters0094-82761944-80072025-07-015213n/an/a10.1029/2025GL117165Asymmetric ENSO Forcing on the South Pacific Meridional ModeCheng Qi0Fan Jia1Key Laboratory of Ocean Observation and Forecasting and Key Laboratory of Ocean Circulation and Waves Institute of Oceanology Chinese Academy of Sciences Qingdao ChinaKey Laboratory of Ocean Observation and Forecasting and Key Laboratory of Ocean Circulation and Waves Institute of Oceanology Chinese Academy of Sciences Qingdao ChinaAbstract The South Pacific Meridional Mode (SPMM) influences El Niño‐Southern Oscillation (ENSO) variability, but whether ENSO triggers SPMM remains unclear. We show that ENSO can induce an in‐phase SPMM event via atmospheric teleconnections, beginning in early boreal summer of the ENSO‐developing year, with a negative asymmetry. Strong La Niña induces negative SPMM more effectively than El Niño induces positive SPMM, due to differences in ENSO teleconnections and their intensity. During boreal summer and fall of strong La Niña, intense transient eddy feedback reshapes the Pacific‐South America pattern into a South Pacific Oscillation‐like pressure dipole, strengthening trade winds and promoting negative SPMM growth, a process absent in El Niño. In boreal winter, stronger La Niña teleconnections sustain negative SPMM into spring. Half of the negative SPMM events co‐occur with negative North Pacific Meridional Mode, contributing to multi‐year La Niña development. These findings advance the understanding of SPMM and its impact on ENSO.https://doi.org/10.1029/2025GL117165ENSOSouth Pacific meridional modemulti‐year La Niñateleconnection
spellingShingle Cheng Qi
Fan Jia
Asymmetric ENSO Forcing on the South Pacific Meridional Mode
Geophysical Research Letters
ENSO
South Pacific meridional mode
multi‐year La Niña
teleconnection
title Asymmetric ENSO Forcing on the South Pacific Meridional Mode
title_full Asymmetric ENSO Forcing on the South Pacific Meridional Mode
title_fullStr Asymmetric ENSO Forcing on the South Pacific Meridional Mode
title_full_unstemmed Asymmetric ENSO Forcing on the South Pacific Meridional Mode
title_short Asymmetric ENSO Forcing on the South Pacific Meridional Mode
title_sort asymmetric enso forcing on the south pacific meridional mode
topic ENSO
South Pacific meridional mode
multi‐year La Niña
teleconnection
url https://doi.org/10.1029/2025GL117165
work_keys_str_mv AT chengqi asymmetricensoforcingonthesouthpacificmeridionalmode
AT fanjia asymmetricensoforcingonthesouthpacificmeridionalmode