RAPID-MOCHA-WBTS Array at 26.5°N
node · earth · Subtropical North Atlantic — 26.5°N section
A trans-basin line of moored instruments across the Atlantic at 26.5°N, from the Bahamas to the African shelf, which has measured the overturning circulation continuously since April 2004. It is a collaboration of the UK National Oceanography Centre, the University of Miami and NOAA. The method is indirect and worth understanding: the array does not measure the overturning directly but sums the Florida Current transport from the submarine cable, the wind-driven Ekman transport from satellite winds, and the mid-ocean geostrophic transport inferred from density profiles at the boundaries. Twenty-plus years in, it remains the longest direct record of any overturning circulation anywhere.
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Evidence · 2
Timeline
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Connections · 3
- Atlantic Meridional Overturning Circulation (AMOC)assesses
- Gulf Streamdepends_on
- Sverdrup (Sv)uses
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Observed changes · 0
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