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Role of the Labrador Current in the Atlantic Meridional Overturning Circulation response to greenhouse warming

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  • Xuan Shan

    (Ocean University of China
    Woods Hole Oceanographic Institution)

  • Shantong Sun

    (Laoshan Laboratory)

  • Lixin Wu

    (Ocean University of China
    Laoshan Laboratory)

  • Michael Spall

    (Woods Hole Oceanographic Institution)

Abstract

Anthropogenic warming is projected to enhance Arctic freshwater exportation into the Labrador Sea. This extra freshwater may weaken deep convection and contribute to the Atlantic Meridional Overturning Circulation (AMOC) decline. Here, by analyzing an unprecedented high-resolution climate model simulation for the 21st century, we show that the Labrador Current strongly restricts the lateral spread of freshwater from the Arctic Ocean into the open ocean such that the freshwater input has a limited role in weakening the overturning circulation. In contrast, in the absence of a strong Labrador Current in a climate model with lower resolution, the extra freshwater is allowed to spread into the interior region and eventually shut down deep convection in the Labrador Sea. Given that the Labrador Sea overturning makes a significant contribution to the AMOC in many climate models, our results suggest that the AMOC decline during the 21st century could be overestimated in these models due to the poorly resolved Labrador Current.

Suggested Citation

  • Xuan Shan & Shantong Sun & Lixin Wu & Michael Spall, 2024. "Role of the Labrador Current in the Atlantic Meridional Overturning Circulation response to greenhouse warming," Nature Communications, Nature, vol. 15(1), pages 1-8, December.
  • Handle: RePEc:nat:natcom:v:15:y:2024:i:1:d:10.1038_s41467-024-51449-9
    DOI: 10.1038/s41467-024-51449-9
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    References listed on IDEAS

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