Historical satellite-derived sea surface temperature (SST) data are re
analyzed with a zebra color palette and a thermal separatrix method. T
he new results from this reanalysis are as follows: a) Thirteen observ
ational sequences of six rings from the Gulf Stream and the Brazil Cur
rent, which have historically been interpreted as solitary vortices or
monopoles are shown to have a dipolar character; b) some of these dip
ole rings have been observed in the open ocean, thereby eliminating th
e possibility that they are sustained by topographic interactions with
the continental slope; c) whether interacting with other features or
evolving as isolated circulations, dipoles are seen to rotate within a
relatively narrow range of approximately 4-8 degrees day(-1) (interac
ting) and 10-15 degrees day(-1) (isolated); and d) feature tracking de
lineates energetic fluid in both vortices and eliminates the possibili
ty of interpreting dipole rings as transient features produced by acti
ve monopoles and patches of entrained fluid.