Bottom water throughflows at the Rio de Janeiro Fracture Zone (22° S) and Rio Grande Fracture Zone (26° S) of the Mid-Atlantic Ridge are identified from hydrographic anomalies observed along 9° W in the Angola Basin. The throughflow water is supplied by a meridional band of cold and fresh water lying against the western flank of the Ridge.
CITATION STYLE
Mercier, H., Weatherly, G. L., & Arhan, M. (2000). Bottom water throughflows at the Rio de Janeiro and Rio Grande Fracture Zones. Geophysical Research Letters, 27(10), 1503–1506. https://doi.org/10.1029/2000GL011402
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