Florida Current transport observations reveal four decades of steady state

The potential weakening of the Atlantic Meridional Overturning Circulation (AMOC) in response to anthropogenic forcing, suggested by climate models, is at the forefront of scientific debate. A key AMOC component, the Florida Current (FC), has been measured using submarine cables between Florida and the Bahamas at 27°N nearly continuously since 1982. A decrease in the FC strength could be indicative of the AMOC weakening. Here, we reassess motion-induced voltages measured on a submarine cable and reevaluate the overall trend in the inferred FC transport. We find that the cable record beginning in 2000 requires a correction for the secular change in the geomagnetic field. This correction removes a spurious trend in the record, revealing that the FC has remained remarkably stable. The recomputed AMOC estimates at ~26.5°N result in a significantly weaker negative trend than that which is apparent in the AMOC time series obtained with the uncorrected FC transports.

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Publication Details

Journal
Nature Communications
Published
2024-09-05
DOI
https://doi.org/10.1038/s41467-024-51879-5
Citations
16
Primary Topic
Atmospheric and Environmental Gas Dynamics
Type
article
Field-Weighted Citation Impact
4.52

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article

Florida Current transport observations reveal four decades of steady state

Ryan H. Smith, Ben Moat, Rigoberto F. García, Molly Baringer et al.
16 citations
Nature Communications
Atmospheric and Environmental Gas Dynamics
4.52
article

Florida Current transport observations reveal four decades of steady state

Ryan H. Smith, Ben Moat, Rigoberto F. García, Molly Baringer, David Smeed, William E. Johns, Denis L. Volkov
article en
16 citations

Abstract

The potential weakening of the Atlantic Meridional Overturning Circulation (AMOC) in response to anthropogenic forcing, suggested by climate models, is at the forefront of scientific debate. A key AMOC component, the Florida Current (FC), has been measured using submarine cables between Florida and the Bahamas at 27°N nearly continuously since 1982. A decrease in the FC strength could be indicative of the AMOC weakening. Here, we reassess motion-induced voltages measured on a submarine cable and reevaluate the overall trend in the inferred FC transport. We find that the cable record beginning in 2000 requires a correction for the secular change in the geomagnetic field. This correction removes a spurious trend in the record, revealing that the FC has remained remarkably stable. The recomputed AMOC estimates at ~26.5°N result in a significantly weaker negative trend than that which is apparent in the AMOC time series obtained with the uncorrected FC transports.

Nature CommunicationsVol. 15(1)
St. Thomas University (US), University of Miami (US), National Oceanography Centre (GB), NOAA Atlantic Oceanographic and Meteorological Laboratories (US)
National Science Foundation, University of Miami, Sight Research UK, National Oceanic and Atmospheric Administration, Natural Environment Research Council, Climate Program Office, Global Ocean Monitoring and Observing Program, NOAA's Atlantic Oceanographic and Meteorological Laboratory
Climate action
Openalex Percentile: Top 5%
Atmospheric and Environmental Gas Dynamics
4.52
DOIOpen Access PDFOpenAlex
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