The Brazil Current is a warm water current that flows south along the Brazilian south coast to the mouth of the Río de la Plata. This current is caused by diversion of a portion of the Atlantic South Equatorial Current from where that current meets the South American continent. It is a western boundary current like the Gulf Stream, and is indeed its southern counterpart; however, it is considerably shallower and weaker.It flows south from the equator to the west wind drift. It joins the Falkland Current at the Argentine Sea, making it a temperate sea.
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“The current of our thoughts made as sudden bends as the river, which was continually opening new prospects to the east or south, but we are aware that rivers flow most rapidly and shallowest at these points.”
—Henry David Thoreau (1817–1862)