Highly variable upper and abyssal overturning cells in the South Atlantic

Highly variable upper and abyssal overturning cells in the South Atlantic

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 stu...

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Bibliographic Details
Main Author: Kersale, Marion (author)
Other Authors: Meinen, Christopher S. (author), Perez, Renellys C. (author), Le Henaff, Matthieu (author), Valla, Daniel (author), Lamont, Tarron (author), Sato, Olga (author), Dong, Shenfu (author), Terre, Thierry (author), van Caspel, Mathias (author), Chidichimo, Maria Paz (author), van den Berg, Marcel (author), Speich, Sabrina (author), Piola, Alberto (author), Campos, Edmo (author), Ansorge, Isabelle (author), Volkov, Denis (author), Lumpkin, Rick (author), Garzoli, Silvia (author)
Format: article
Published: 2020
Online Access:http://hdl.handle.net/11073/19569
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http://hdl.handle.net/11073/19569

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