The East Auckland Current (EAUC) was investigated in 1994-95 using dat
a from three CTD surveys (conductivity, temperature, depth) and moored
current meters. The strength and position of the EAUC was found to be
highly variable with most of the current re-circulating around an ant
icyclonic eddy north-east of North Cape-the North Cape Eddy. The posit
ion and intensity of this eddy changed resulting in complex flow patte
rns with a south-east flowing EAUC not always present as a contiguous
feature. The current meter data showed a high level of mesoscale varia
bility with low spatial coherence, suggesting that the along shore cor
relation length scale was c. 100 km in this current system. Near North
Cape, a persistent but variable counter-current was found inshore of
the EAUC. To the south-east a permanent anticyclonic East Cape Eddy fo
und north of East Cape appears to dominate the flow field and the gene
sis of the East Cape Current.