In the austral winter of 1993, during a COROAS hydrographic cruise in the S
outh Brasil Eight (SBB), an unexpected mass of cold and fresh water was obs
erved on the continental shelf near 23 degrees S. Subsequent analyses of di
fferent data sets suggested that the origin of that water was probably the
Argentine continental shelf, near the Rio de la Plata mouth. In this articl
e, a 13-year time series of AVHRR Sea Surface Temperature anomalies is anal
ysed to investigate the occurrence of this phenomenon in other periods. The
results of these analyses and a good correlation with the Southern Oscilla
tion Index suggest that the penetration of these waters into the SBB occurs
in a frequency that may be associated with ENSO events.