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Basin-Wide Oceanographic Array Bridges the South Atlantic ArchiMer
Ansorge, Isabelle J.; Baringer, Molly; Campos, Edmo J.d.; Dong, S.; Fine, R.a.; Garzoli, Silvia L.; Goni, Gustavo; Meinen, Christopher S.; Perez, R.c.; Piola, Alberto R.; Roberts, M.j.; Speich, Sabrina; Sprintall, J.; Terre Terrillon, Thierry; Van Den Berg, M.a..
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].
Tipo: Text Palavras-chave: South Atlantic; Meridional Overturning Circulation; CPIES.
Ano: 2014 URL: http://archimer.ifremer.fr/doc/00175/28609/27109.pdf
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Highly variable upper and abyssal overturning cells in the South Atlantic ArchiMer
Kersalé, M.; Meinen, C. S.; Perez, Rc; Le Hénaff, M.; Valla, D.; Lamont, T.; Sato, O. T.; Dong, S.; Terre-terrillon, Thierry; Van Caspel, M.; Chidichimo, M. P.; Van Den Berg, M.; Speich, S.; Piola, A. R.; Campos, E. J. D.; Ansorge, I.; Volkov, D. L.; Lumpkin, R.; Garzoli, S. L..
The Meridional Overturning Circulation (MOC) is a primary mechanism driving oceanic heat redistribution on Earth, thereby affecting Earth’s climate and weather. However, the full-depth structure and variability of the MOC are still poorly understood, particularly in the South Atlantic. This study presents unique multiyear records of the oceanic volume transport of both the upper (<~3100 meters) and abyssal (>~3100 meters) overturning cells based on daily moored measurements in the South Atlantic at 34.5°S. The vertical structure of the time-mean flows is consistent with the limited historical observations. Both the upper and abyssal cells exhibit a high degree of variability relative to the temporal means at time scales, ranging from a few days to a...
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Ano: 2020 URL: https://archimer.ifremer.fr/doc/00645/75705/76614.pdf
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