Assessment of the global ocean heat content and North Atlantic heat transport over 1993–2020

Understanding changes in global ocean heat content (OHC) is essential for investigating Earth’s energy imbalance and climate change. OHC trends are assessed using four state-of-the-art ocean reanalyses and one objective analysis. The spatial OHC trend patterns captured by reanalyses are consistent with each other, but sensitive to the selected time period. A higher proportion of heat uptake in the 100–2000 m sub-surface layer over 2001–2010 than 1994–2000 contributed to the temporary slowdown in global surface warming. The North Atlantic meridional overturning circulation (MOC) and heat transport show better agreement with RAPID observations compared with previous studies. Zonal mean OHC trends in the North Atlantic over 40–60 °N differ for the MOC increasing (2000–2004) and decreasing periods (2005–2010) and OHC increases are more concentrated between 30 and 40 °N in the later MOC increasing period (2011–2022). These results do not support previous studies suggesting that MOC changes are reducing Earth’s mean surface warming.

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Publication Details

Journal
npj Climate and Atmospheric Science
Published
2024-12-19
DOI
https://doi.org/10.1038/s41612-024-00860-6
Citations
5
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
1.41

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article

Assessment of the global ocean heat content and North Atlantic heat transport over 1993–2020

Michael Mayer, Zhenya Song, Qianye Su, Jiandong Li et al.
5 citations
npj Climate and Atmospheric Science
Climate variability and models
1.41
article

Assessment of the global ocean heat content and North Atlantic heat transport over 1993–2020

Michael Mayer, Zhenya Song, Qianye Su, Jiandong Li, Richard P. Allan, Fangli Qiao, Hongzhou Xu, Susanna Winkelbauer, Liang Jin, Xiaoqing Liao, Ke Yang, Ning Cao, Lijing Cheng, Yuying Pan, Chunlei Liu, Liang Zhao
article en
5 citations

Abstract

Understanding changes in global ocean heat content (OHC) is essential for investigating Earth’s energy imbalance and climate change. OHC trends are assessed using four state-of-the-art ocean reanalyses and one objective analysis. The spatial OHC trend patterns captured by reanalyses are consistent with each other, but sensitive to the selected time period. A higher proportion of heat uptake in the 100–2000 m sub-surface layer over 2001–2010 than 1994–2000 contributed to the temporary slowdown in global surface warming. The North Atlantic meridional overturning circulation (MOC) and heat transport show better agreement with RAPID observations compared with previous studies. Zonal mean OHC trends in the North Atlantic over 40–60 °N differ for the MOC increasing (2000–2004) and decreasing periods (2005–2010) and OHC increases are more concentrated between 30 and 40 °N in the later MOC increasing period (2011–2022). These results do not support previous studies suggesting that MOC changes are reducing Earth’s mean surface warming.

npj Climate and Atmospheric ScienceVol. 7(1)
University of Vienna (AT), Chinese Academy of Sciences (CN), Ministry of Natural Resources (CN), Institute of Oceanology (CN), First Institute of Oceanography (CN), National Centre for Earth Observation (GB), Institute of Atmospheric Physics (CN), Institute of Deep-Sea Science and Engineering (CN), University of Reading (GB), Guangdong Ocean University (CN)
Sight Research UK, University of Reading, National Natural Science Foundation of China, Chinese Academy of Sciences, Austrian Science Fund, Institute of Atmospheric Physics, Chinese Academy of Sciences, Guangdong Ocean University, Natural Environment Research Council
Life below water
Openalex Percentile: Top 18%
Climate variability and models
1.41
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