Changes in Atmospheric Convection Over the Indo‐Pacific Warm Pool and Coupled IOD and ENSO Patterns During the Last Glacial Maximum

Abstract This study investigates how the convection over the Indo‐Pacific Warm Pool responds to the Last Glacial Maximum conditions. Paleoproductivity records that can indicate seasonal wind dynamics are combined with modeling data. Seasonal southeasterly and northeasterly winds off Sumatra are both strengthened, meanwhile, anomalous westerly winds occur over the western Celebes Sea. This reflects a zonal “tripole” pattern of the changed convection that is weakened over the exposed Sunda and Sahul shelves and strengthened over the eastern equatorial Indian Ocean and western equatorial Pacific. Model results suggest that lower sea levels and larger ice sheets are responsible for these changes. Coupled with the changed atmospheric circulation, a positive Indian Ocean Dipole‐like mean state forms in the Indian Ocean. The Pacific likely exhibits an “eastern Pacific La Niña”‐like superposed by a “central Pacific El‐Niño”‐like mean state. Under such configuration, the Indian Ocean Dipole and El Niño‐Southern Oscillation variability probably strengthen.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-03-17
DOI
https://doi.org/10.1029/2024gl112276
Citations
2
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
2.60

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article

Changes in Atmospheric Convection Over the Indo‐Pacific Warm Pool and Coupled IOD and ENSO Patterns During the Last Glacial Maximum

Xinquan Zhou, Xiaobo Jin, Franck Bassinot, Eva Moréno et al.
2 citations
Geophysical Research Letters
Geology and Paleoclimatology Research
2.60
article

Changes in Atmospheric Convection Over the Indo‐Pacific Warm Pool and Coupled IOD and ENSO Patterns During the Last Glacial Maximum

Xinquan Zhou, Xiaobo Jin, Franck Bassinot, Eva Moréno, Chuanlian Liu, Stéphanie Duchamp‐Alphonse, Xiaoxu Shi, Luc Beaufort
article en
2 citations

Abstract

Abstract This study investigates how the convection over the Indo‐Pacific Warm Pool responds to the Last Glacial Maximum conditions. Paleoproductivity records that can indicate seasonal wind dynamics are combined with modeling data. Seasonal southeasterly and northeasterly winds off Sumatra are both strengthened, meanwhile, anomalous westerly winds occur over the western Celebes Sea. This reflects a zonal “tripole” pattern of the changed convection that is weakened over the exposed Sunda and Sahul shelves and strengthened over the eastern equatorial Indian Ocean and western equatorial Pacific. Model results suggest that lower sea levels and larger ice sheets are responsible for these changes. Coupled with the changed atmospheric circulation, a positive Indian Ocean Dipole‐like mean state forms in the Indian Ocean. The Pacific likely exhibits an “eastern Pacific La Niña”‐like superposed by a “central Pacific El‐Niño”‐like mean state. Under such configuration, the Indian Ocean Dipole and El Niño‐Southern Oscillation variability probably strengthen.

Geophysical Research LettersVol. 52(6)
Tongji University (CN), Centre National de la Recherche Scientifique (FR), Université de Versailles Saint-Quentin-en-Yvelines (FR), Aix-Marseille Université (FR), Commissariat à l'Énergie Atomique et aux Énergies Alternatives (FR), Université Paris-Saclay (FR), Sorbonne Université (FR), Centre de Recherche et d’Enseignement de Géosciences de l’Environnement (FR), Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) (CN), Laboratoire des Sciences du Climat et de l'Environnement (FR), CEA Paris-Saclay (FR), Geosciences Paris-Saclay (FR), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (FR), Institut de Recherche pour le Développement (FR), Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) (CN)
China Scholarship Council
Life below water
Openalex Percentile: Top 13%
Geology and Paleoclimatology Research
2.60
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