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Modulation of the interdecadal trend of global surface air temperature by sea surface temperature over multiple ocean basins

Bibliographic Data

ID15544797
AuthorsYidan Xu (0000-0002-8977-8331, China Meteorological Administration, corresponding author), Jianping Li (0000-0003-4976-4119, Laoshan Laboratory), Jiaxu Guo (0000-0001-8348-9283, Shenyang Aerospace University), Jing Sun (0000-0003-0850-322X, China Meteorological Administration), Shuai Deng (0000-0002-2365-1944, China Meteorological Administration), Haohuan Fu (0000-0002-6982-2235, University Town of Shenzhen), Lanning Wang (0000-0003-4400-0064, Beijing Normal University), Wei Xue (0000-0002-4942-7748, Tsinghua University)
Year2025
Volume20
Issue4
Pages044010-044010
Publication date2025-03-06
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/adbd56
OpenAlexW4408177494
LanguageEN
References cited46

Since the 20th century, accompanied by a long-term warming trend, the global surface air temperature (SAT) has exhibited distinct interdecadal oscillations. The period from 1910 to 2012 can be divided into four phases, including two rapid warming (1910–1945 and 1975–1998) and two warming slowdown (1940–1975 and 1998–2012) periods. This study explores the spatiotemporal characteristics of the interdecadal trends in global SAT under the influence of sea surface temperature (SST) on a multi-basin scale. Here, we have accumulated the numerical simulated SAT anomalies under the forcing of historical SST in the selected ocean basins. The results indicate that multi-basin SSTs collectively govern the spatiotemporal variations and interdecadal trends of SATs during rapid warming periods. SSTs in the Indian Ocean, North Atlantic, and western Pacific can affect the spatiotemporal interdecadal trends of SAT during 1940–1975. SSTs in the eastern tropical Pacific and North Pacific can modify the SAT spatiotemporal trends during 1998–2012. Considering the nonlinear interactions between different oceanic regions, the SAT forced by the collective SSTs in the six ocean basins shows high consistency with observation. This indicates that the combined effects of SSTs in the six ocean basins are key reasons for global SAT interdecadal change in 1910–2012

Air temperature · Atmospheric sciences · Climate change · Climatology · Modulation (music · Physics · Sea surface temperature · Surface (topology · Surface air temperature · Arctic and Antarctic ice dynamics · Environmental Science · Oceanographic and Atmospheric Processes · Geology · Oceanography

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