Abstract
The northward flow of the upper limb of the Atlantic Meridional Overturning Circulation (AMOC) is fed by waters entering the South Atlantic from the Indian Ocean mainly via the Agulhas Current (AC) system and by waters entering from the Pacific through Drake Passage (DP), commonly referred to as the "warm" and "cold" water routes, respectively. However, there is no final consensus on the relative importance of these two routes for the upper limb's volume transport and thermohaline properties. In this study we revisited the AC and DP contributions by performing Lagrangian analyses between the two source regions and the North Brazil Current (NBC) at 6°S in a realistically forced high-resolution (1/20
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CITATION STYLE
Rühs, S., Schwarzkopf, F. U., Speich, S., & Biastoch, A. (2019). Cold vs. warm water route-sources for the upper limb of the Atlantic Meridional Overturning Circulation revisited in a high-resolution ocean model. Ocean Science, 15(3), 489–512. https://doi.org/10.5194/os-15-489-2019
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