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Two centuries of limited variability in subtropical North Atlantic thermocline ventilation

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  • Nathalie F. Goodkin

    (University of Hong Kong)

  • Ellen R. M. Druffel

    (University of California, Irvine, California 92697, USA.)

  • Konrad A. Hughen

    (Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA.)

  • Scott C. Doney

    (Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA.)

Abstract

Ventilation and mixing of oceanic gyres is important to ocean-atmosphere heat and gas transfer, and to mid-latitude nutrient supply. The rates of mode water formation are believed to impact climate and carbon exchange between the surface and mid-depth water over decadal periods. Here, a record of 14C/12C (1780–1940), which is a proxy for vertical ocean mixing, from an annually banded coral from Bermuda, shows limited inter-annual variability and a substantial Suess Effect (the decrease in 14C/12C since 1900). The Sargasso Sea mixing rates between the surface and thermocline varied minimally over the past two centuries, despite changes to mean-hemispheric climate, including the Little Ice Age and variability in the North Atlantic Oscillation. This result indicates that regional formation rates of sub-tropical mode water are stable over decades, and that anthropogenic carbon absorbed by the ocean does not return to the surface at a variable rate.

Suggested Citation

  • Nathalie F. Goodkin & Ellen R. M. Druffel & Konrad A. Hughen & Scott C. Doney, 2012. "Two centuries of limited variability in subtropical North Atlantic thermocline ventilation," Nature Communications, Nature, vol. 3(1), pages 1-6, January.
  • Handle: RePEc:nat:natcom:v:3:y:2012:i:1:d:10.1038_ncomms1811
    DOI: 10.1038/ncomms1811
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