Basin-wide oceanographic array bridges the South Atlantic

I. J. Ansorge, M. O. Baringer, E. J.D. Campos, S. Dong, R. A. Fine, S. L. Garzoli, G. Goni, C. S. Meinen, R. C. Perez, A. R. Piola, M. J. Roberts, S. Speich, J. Sprintall, T. Terre, M. A. Van Den Berg

Research output: Contribution to journalArticlepeer-review

31 Scopus citations


The meridional overturning circulation (MOC) is a global system of surface, intermediate, and deep ocean currents. The MOC connects the surface layer of the ocean and the atmosphere with the huge reservoir of the deep sea and is the primary mechanism for transporting heat, freshwater, and carbon between ocean basins. Climate models show that past changes in the strength of the MOC were linked to historical climate variations. Further research suggests that the MOC will continue to modulate climate change scenarios on time scales ranging from decades to centuries [Latif et al., 2006].

Original languageEnglish (US)
Pages (from-to)53-54
Number of pages2
Issue number6
StatePublished - Feb 11 2014


  • Meridional Overturning Circulation
  • South Atlantic

ASJC Scopus subject areas

  • Earth and Planetary Sciences(all)


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