Inter-basin contrast in the Southern Ocean warming

The Southern Ocean (SO) is a major contributor to global ocean heat uptake, exhibiting deep-reaching warming trends within the 35°S-55°S band. Here, we reveal a notable inter-basin contrast in the SO warming rates. Over the past six decades, the warming of the 0-700 m Atlantic-Indian sector was 40.0 ± 5.7% faster than the Pacific sector, nearly doubling at ~44°S. Ocean-only and coupled model experiments suggest that this basin-scale contrast arises from alterations in wind-driven heat redistribution rather than surface heating. Specifically, the intensification and poleward migration of westerly winds are more prominent in the Atlantic-Indian sector, leading to stronger upper-layer heat convergence. The inter-basin warming contrast is projected to persist and amplify throughout the remainder of the 21<sup>st</sup> century. This study highlights the inter-basin contrast in the past and future SO warming, with useful implications for understanding regional changes in the SO climate, ice mass, and marine ecosystems.

Authors

Institutions

Publication Details

Journal
Nature Communications
Published
2025-10-13
DOI
https://doi.org/10.1038/s41467-025-64112-8
Citations
1
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
1.11

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Inter-basin contrast in the Southern Ocean warming

Jia‐Rui Shi, Yuanyuan Song, Kai Ge, Fan Wang et al.
1 citations
Nature Communications
Climate variability and models
1.11
article

Inter-basin contrast in the Southern Ocean warming

Jia‐Rui Shi, Yuanyuan Song, Kai Ge, Fan Wang, Aixue Hu, Gaël Forget, Qian Li, Xiaodan Chen, Yuanlong Li
article en
1 citations

Abstract

The Southern Ocean (SO) is a major contributor to global ocean heat uptake, exhibiting deep-reaching warming trends within the 35°S-55°S band. Here, we reveal a notable inter-basin contrast in the SO warming rates. Over the past six decades, the warming of the 0-700 m Atlantic-Indian sector was 40.0 ± 5.7% faster than the Pacific sector, nearly doubling at ~44°S. Ocean-only and coupled model experiments suggest that this basin-scale contrast arises from alterations in wind-driven heat redistribution rather than surface heating. Specifically, the intensification and poleward migration of westerly winds are more prominent in the Atlantic-Indian sector, leading to stronger upper-layer heat convergence. The inter-basin warming contrast is projected to persist and amplify throughout the remainder of the 21<sup>st</sup> century. This study highlights the inter-basin contrast in the past and future SO warming, with useful implications for understanding regional changes in the SO climate, ice mass, and marine ecosystems.

Nature CommunicationsVol. 16(1)
Florida State University (US), NSF National Center for Atmospheric Research (US), Fudan University (CN), Courant Institute of Mathematical Sciences (US), Institute of Oceanology (CN), Qingdao National Laboratory for Marine Science and Technology (CN), NSF NCAR Climate and Global Dynamics Laboratory (US), New York University (US), Massachusetts Institute of Technology (US), Woods Hole Oceanographic Institution (US)
National Science Foundation, U.S. Department of Energy, National Aeronautics and Space Administration, National Natural Science Foundation of China, Chinese Academy of Sciences, Nuclear Safety and Security Commission, Institute of Oceanology, Chinese Academy of Sciences
Openalex Percentile: Top 19%
Climate variability and models
1.11
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.