Enhanced ocean heat storage efficiency during the last deglaciation

Proxy reconstructions suggest that increasing global mean sea surface temperature (GMSST) during the last deglaciation was accompanied by a comparable or greater increase in global mean ocean temperature (GMOT), corresponding to a large heat storage efficiency (HSE; ∆GMOT/∆GMSST). An increased GMOT is commonly attributed to surface warming at sites of deepwater formation, but winter sea ice covered much of these source areas during the last deglaciation, which would imply an HSE much less than 1. Here, we use climate model simulations and proxy-based reconstructions of ocean temperature changes to show that an increased deglacial HSE is achieved by warming of intermediate-depth waters forced by mid-latitude surface warming in response to greenhouse gas and ice sheet forcing as well as by reduced Atlantic meridional overturning circulation associated with meltwater forcing. These results, which highlight the role of surface warming and oceanic circulation changes, have implications for our understanding of long-term ocean heat storage change.

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Publication Details

Journal
Science Advances
Published
2024-09-20
DOI
https://doi.org/10.1126/sciadv.adp5156
Citations
9
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
3.39

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article

Enhanced ocean heat storage efficiency during the last deglaciation

Jiuyou Lu, S. Sanchez, Chenyu Zhu, Peter U. Clark et al.
9 citations
Science Advances
Geology and Paleoclimatology Research
3.39
article

Enhanced ocean heat storage efficiency during the last deglaciation

Jiuyou Lu, S. Sanchez, Chenyu Zhu, Peter U. Clark, Chengfei He, Lingfeng Wan, Lijing Cheng, Zhengyu Liu, Lingwei Li, Shaoqing Zhang
article en
9 citations

Abstract

Proxy reconstructions suggest that increasing global mean sea surface temperature (GMSST) during the last deglaciation was accompanied by a comparable or greater increase in global mean ocean temperature (GMOT), corresponding to a large heat storage efficiency (HSE; ∆GMOT/∆GMSST). An increased GMOT is commonly attributed to surface warming at sites of deepwater formation, but winter sea ice covered much of these source areas during the last deglaciation, which would imply an HSE much less than 1. Here, we use climate model simulations and proxy-based reconstructions of ocean temperature changes to show that an increased deglacial HSE is achieved by warming of intermediate-depth waters forced by mid-latitude surface warming in response to greenhouse gas and ice sheet forcing as well as by reduced Atlantic meridional overturning circulation associated with meltwater forcing. These results, which highlight the role of surface warming and oceanic circulation changes, have implications for our understanding of long-term ocean heat storage change.

Science AdvancesVol. 10(38)
Oregon State University (US), University of Miami (US), Nanjing Normal University (CN), Institute of Arctic and Alpine Research (US), University of Colorado Boulder (US), Chinese Academy of Sciences (CN), China University of Geosciences (Beijing) (CN), Institute of Atmospheric Physics (CN), Laoshan Laboratory, The Ohio State University (US), Ocean University of China (CN)
National Science Foundation, EarthLab, University of Washington
Life below water
Openalex Percentile: Top 7%
Geology and Paleoclimatology Research
3.39
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