North Atlantic-Pacific salinity contrast enhanced by wind and ocean warming
High salinities in the Atlantic and low salinities in the Pacific are critical ocean features, impacting ocean circulations and climate. Here, using observational data, we reveal that the Atlantic-Pacific salinity contrast has amplified during the past half-century. Notably, in the 0-800 m, 20 degre...
Published in: | Nature Climate Change |
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ftchinacasciocas:oai:ir.qdio.ac.cn:337002/186469 2024-09-30T14:39:17+00:00 North Atlantic-Pacific salinity contrast enhanced by wind and ocean warming Lu, Ying Li, Yuanlong Lin, Pengfei Cheng, Lijing Ge, Kai Liu, Hailong Duan, Jing Wang, Fan 2024-06-28 http://ir.qdio.ac.cn/handle/337002/186469 https://doi.org/10.1038/s41558-024-02033-y 英语 eng NATURE PORTFOLIO NATURE CLIMATE CHANGE http://ir.qdio.ac.cn/handle/337002/186469 doi:10.1038/s41558-024-02033-y Environmental Sciences & Ecology Meteorology & Atmospheric Sciences Environmental Sciences Environmental Studies GLOBAL OCEAN SURFACE SALINITY TEMPERATURE TRENDS MECHANISMS DECLINE RATES CYCLE FLUX 期刊论文 2024 ftchinacasciocas https://doi.org/10.1038/s41558-024-02033-y 2024-09-05T23:42:51Z High salinities in the Atlantic and low salinities in the Pacific are critical ocean features, impacting ocean circulations and climate. Here, using observational data, we reveal that the Atlantic-Pacific salinity contrast has amplified during the past half-century. Notably, in the 0-800 m, 20 degrees-40 degrees N band, the Atlantic-Pacific salinity contrast increased by 5.9% +/- 0.6% since 1965. A decomposition of heaving and spicing modes suggests vital contributions of wind and ocean warming, in addition to known surface freshwater fluxes. Specifically, ocean surface warming leads to poleward migration of thermocline outcrop zones, while surface wind changes cause upper-layer convergence in mid-latitudes. These processes lead to substantial upper-layer salinity increases in the North Atlantic but have much weaker signatures in the North Pacific, determined by the inter-basin difference in climatological salinities. This work highlights the complexity of ocean salinity response to climate change, underscoring the unexpected importance of wind- and heat-driven processes in the Atlantic-Pacific salinity contrast. Ocean salinity changes are thought to be dominated by freshwater fluxes. Here the authors show that amplification of the Atlantic-Pacific salinity contrast also involves wind- and ocean warming-driven processes, with larger salinity increases in the North Atlantic, relative to the North Pacific. Report North Atlantic Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR Pacific Nature Climate Change 14 7 723 731 |
institution |
Open Polar |
collection |
Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR |
op_collection_id |
ftchinacasciocas |
language |
English |
topic |
Environmental Sciences & Ecology Meteorology & Atmospheric Sciences Environmental Sciences Environmental Studies GLOBAL OCEAN SURFACE SALINITY TEMPERATURE TRENDS MECHANISMS DECLINE RATES CYCLE FLUX |
spellingShingle |
Environmental Sciences & Ecology Meteorology & Atmospheric Sciences Environmental Sciences Environmental Studies GLOBAL OCEAN SURFACE SALINITY TEMPERATURE TRENDS MECHANISMS DECLINE RATES CYCLE FLUX Lu, Ying Li, Yuanlong Lin, Pengfei Cheng, Lijing Ge, Kai Liu, Hailong Duan, Jing Wang, Fan North Atlantic-Pacific salinity contrast enhanced by wind and ocean warming |
topic_facet |
Environmental Sciences & Ecology Meteorology & Atmospheric Sciences Environmental Sciences Environmental Studies GLOBAL OCEAN SURFACE SALINITY TEMPERATURE TRENDS MECHANISMS DECLINE RATES CYCLE FLUX |
description |
High salinities in the Atlantic and low salinities in the Pacific are critical ocean features, impacting ocean circulations and climate. Here, using observational data, we reveal that the Atlantic-Pacific salinity contrast has amplified during the past half-century. Notably, in the 0-800 m, 20 degrees-40 degrees N band, the Atlantic-Pacific salinity contrast increased by 5.9% +/- 0.6% since 1965. A decomposition of heaving and spicing modes suggests vital contributions of wind and ocean warming, in addition to known surface freshwater fluxes. Specifically, ocean surface warming leads to poleward migration of thermocline outcrop zones, while surface wind changes cause upper-layer convergence in mid-latitudes. These processes lead to substantial upper-layer salinity increases in the North Atlantic but have much weaker signatures in the North Pacific, determined by the inter-basin difference in climatological salinities. This work highlights the complexity of ocean salinity response to climate change, underscoring the unexpected importance of wind- and heat-driven processes in the Atlantic-Pacific salinity contrast. Ocean salinity changes are thought to be dominated by freshwater fluxes. Here the authors show that amplification of the Atlantic-Pacific salinity contrast also involves wind- and ocean warming-driven processes, with larger salinity increases in the North Atlantic, relative to the North Pacific. |
format |
Report |
author |
Lu, Ying Li, Yuanlong Lin, Pengfei Cheng, Lijing Ge, Kai Liu, Hailong Duan, Jing Wang, Fan |
author_facet |
Lu, Ying Li, Yuanlong Lin, Pengfei Cheng, Lijing Ge, Kai Liu, Hailong Duan, Jing Wang, Fan |
author_sort |
Lu, Ying |
title |
North Atlantic-Pacific salinity contrast enhanced by wind and ocean warming |
title_short |
North Atlantic-Pacific salinity contrast enhanced by wind and ocean warming |
title_full |
North Atlantic-Pacific salinity contrast enhanced by wind and ocean warming |
title_fullStr |
North Atlantic-Pacific salinity contrast enhanced by wind and ocean warming |
title_full_unstemmed |
North Atlantic-Pacific salinity contrast enhanced by wind and ocean warming |
title_sort |
north atlantic-pacific salinity contrast enhanced by wind and ocean warming |
publisher |
NATURE PORTFOLIO |
publishDate |
2024 |
url |
http://ir.qdio.ac.cn/handle/337002/186469 https://doi.org/10.1038/s41558-024-02033-y |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
NATURE CLIMATE CHANGE http://ir.qdio.ac.cn/handle/337002/186469 doi:10.1038/s41558-024-02033-y |
op_doi |
https://doi.org/10.1038/s41558-024-02033-y |
container_title |
Nature Climate Change |
container_volume |
14 |
container_issue |
7 |
container_start_page |
723 |
op_container_end_page |
731 |
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1811641869219659776 |