The current is an equatorward flowing current that carries cold and relatively fresh subantarctic water. The Falkland Current is a branch off of the Antarctic Circumpolar Current. It transports between 60 and 90 Sverdrups of water with speeds ranging from a half a meter to a meter per second. Hydrographic data in this area is very scarce and thus various hydrographic variables have a great deal of error. It is interesting to note that the Falkland Current is not simply a surface current like the Brazil Current but actually extends all the way to the sea-floor. Typical temperatures for the current are around 6 °C, with a salinity of 33.5–34.5 psu.
^Vivier, F. and C. Provost, 1999b: Volume transport of the Falkland Current: Can the flow be monitored by TOPEX/POSEIDON ? Journal of Geophysical Research, 104, 21105-21122.
^Vigan, X., C. Provost, and G. Podesta, 2000: Sea surface velocities from sea surface temperature image sequences 2. Application to the Brazil-Malvinas Confluence area. Journal of Geophysical Research, 105, 19515-19534.