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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محفوظ في:
التفاصيل البيبلوغرافية
المؤلف الرئيسي: Kersale, Marion (author)
مؤلفون آخرون: 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)
التنسيق: article
منشور في: 2020
الوصول للمادة أونلاين:http://hdl.handle.net/11073/19569
الوسوم: إضافة وسم
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الانترنت

http://hdl.handle.net/11073/19569

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