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20th century cooling of the deep ocean contributed to delayed acceleration of Earth’s energy imbalance

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  • A. Bagnell

    (University of California)

  • T. DeVries

    (University of California
    University of California)

Abstract

The historical evolution of Earth’s energy imbalance can be quantified by changes in the global ocean heat content. However, historical reconstructions of ocean heat content often neglect a large volume of the deep ocean, due to sparse observations of ocean temperatures below 2000 m. Here, we provide a global reconstruction of historical changes in full-depth ocean heat content based on interpolated subsurface temperature data using an autoregressive artificial neural network, providing estimates of total ocean warming for the period 1946-2019. We find that cooling of the deep ocean and a small heat gain in the upper ocean led to no robust trend in global ocean heat content from 1960-1990, implying a roughly balanced Earth energy budget within −0.16 to 0.06 W m−2 over most of the latter half of the 20th century. However, the past three decades have seen a rapid acceleration in ocean warming, with the entire ocean warming from top to bottom at a rate of 0.63 ± 0.13 W m−2. These results suggest a delayed onset of a positive Earth energy imbalance relative to previous estimates, although large uncertainties remain.

Suggested Citation

  • A. Bagnell & T. DeVries, 2021. "20th century cooling of the deep ocean contributed to delayed acceleration of Earth’s energy imbalance," Nature Communications, Nature, vol. 12(1), pages 1-10, December.
  • Handle: RePEc:nat:natcom:v:12:y:2021:i:1:d:10.1038_s41467-021-24472-3
    DOI: 10.1038/s41467-021-24472-3
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    Cited by:

    1. Zhi Li & Matthew H. England & Sjoerd Groeskamp, 2023. "Recent acceleration in global ocean heat accumulation by mode and intermediate waters," Nature Communications, Nature, vol. 14(1), pages 1-14, December.
    2. Andrea Storto & Chunxue Yang, 2024. "Acceleration of the ocean warming from 1961 to 2022 unveiled by large-ensemble reanalyses," Nature Communications, Nature, vol. 15(1), pages 1-11, December.

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