Paleoclimate proxy records suggest reduced tropical Pacific zonal asymmetry under sustained global warming

Abstract Pronounced model-observation discrepancies in the changes of tropical Pacific zonal sea surface temperature gradient during the satellite era imply systematic model deficiencies. However, the relatively short high-quality instrumental record hampers robustly determining the response of trop...

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Main Authors: Eui-Seok Chung, Seong-Joong Kim, Keith B. Rodgers, Sang-Yoon Jun, Joo-Hong Kim, Sun-Seon Lee, Kyung-Sook Yun
Format: Article
Language:English
Published: Nature Portfolio 2025-02-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-025-02039-0
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author Eui-Seok Chung
Seong-Joong Kim
Keith B. Rodgers
Sang-Yoon Jun
Joo-Hong Kim
Sun-Seon Lee
Kyung-Sook Yun
author_facet Eui-Seok Chung
Seong-Joong Kim
Keith B. Rodgers
Sang-Yoon Jun
Joo-Hong Kim
Sun-Seon Lee
Kyung-Sook Yun
author_sort Eui-Seok Chung
collection DOAJ
description Abstract Pronounced model-observation discrepancies in the changes of tropical Pacific zonal sea surface temperature gradient during the satellite era imply systematic model deficiencies. However, the relatively short high-quality instrumental record hampers robustly determining the response of tropical Pacific sea surface temperature to greenhouse gas increases. By adopting paleoclimate proxy records along with a series of climate model simulations, here we show that the zonal gradient is likely to decrease under sustained strong forcing. Paleoclimate proxy records indicate an overall increase of the zonal gradient over time, which has been accompanied by global-mean cooling associated with decreasing carbon dioxide concentrations. Model simulations are found to broadly reproduce the distinct contrast between warmer high carbon dioxide climates and the opposite climates, albeit with large inter-model discrepancy. The qualitative agreement among paleoclimate proxy records and modeled representations therefore lends some important credence to the sign of model-projected future tropical Pacific mean state change.
format Article
id doaj-art-f73390cdd2b444768abb34372147a83c
institution Kabale University
issn 2662-4435
language English
publishDate 2025-02-01
publisher Nature Portfolio
record_format Article
series Communications Earth & Environment
spelling doaj-art-f73390cdd2b444768abb34372147a83c2025-02-09T12:56:04ZengNature PortfolioCommunications Earth & Environment2662-44352025-02-016111110.1038/s43247-025-02039-0Paleoclimate proxy records suggest reduced tropical Pacific zonal asymmetry under sustained global warmingEui-Seok Chung0Seong-Joong Kim1Keith B. Rodgers2Sang-Yoon Jun3Joo-Hong Kim4Sun-Seon Lee5Kyung-Sook Yun6Division of Ocean and Atmosphere Sciences, Korea Polar Research InstituteKOPRI School, University of Science and TechnologyWPI-Advanced Institute for Marine Ecosystem Change, Tohoku UniversityDivision of Ocean and Atmosphere Sciences, Korea Polar Research InstituteDivision of Ocean and Atmosphere Sciences, Korea Polar Research InstituteCenter for Climate Physics, Institute for Basic ScienceCenter for Climate Physics, Institute for Basic ScienceAbstract Pronounced model-observation discrepancies in the changes of tropical Pacific zonal sea surface temperature gradient during the satellite era imply systematic model deficiencies. However, the relatively short high-quality instrumental record hampers robustly determining the response of tropical Pacific sea surface temperature to greenhouse gas increases. By adopting paleoclimate proxy records along with a series of climate model simulations, here we show that the zonal gradient is likely to decrease under sustained strong forcing. Paleoclimate proxy records indicate an overall increase of the zonal gradient over time, which has been accompanied by global-mean cooling associated with decreasing carbon dioxide concentrations. Model simulations are found to broadly reproduce the distinct contrast between warmer high carbon dioxide climates and the opposite climates, albeit with large inter-model discrepancy. The qualitative agreement among paleoclimate proxy records and modeled representations therefore lends some important credence to the sign of model-projected future tropical Pacific mean state change.https://doi.org/10.1038/s43247-025-02039-0
spellingShingle Eui-Seok Chung
Seong-Joong Kim
Keith B. Rodgers
Sang-Yoon Jun
Joo-Hong Kim
Sun-Seon Lee
Kyung-Sook Yun
Paleoclimate proxy records suggest reduced tropical Pacific zonal asymmetry under sustained global warming
Communications Earth & Environment
title Paleoclimate proxy records suggest reduced tropical Pacific zonal asymmetry under sustained global warming
title_full Paleoclimate proxy records suggest reduced tropical Pacific zonal asymmetry under sustained global warming
title_fullStr Paleoclimate proxy records suggest reduced tropical Pacific zonal asymmetry under sustained global warming
title_full_unstemmed Paleoclimate proxy records suggest reduced tropical Pacific zonal asymmetry under sustained global warming
title_short Paleoclimate proxy records suggest reduced tropical Pacific zonal asymmetry under sustained global warming
title_sort paleoclimate proxy records suggest reduced tropical pacific zonal asymmetry under sustained global warming
url https://doi.org/10.1038/s43247-025-02039-0
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