The Balearic Basin is defined as a wide region of the western Mediterr
anean located in between the Liguro-Provencal and Algerian basins. The
dynamics of the Liguro-Provencal Basin, in the north, is dominated by
the dense water formation process associated with a permanent circula
tion along the continental slope: the Northern Current. The Algerian B
asin, in the south, is dominated by intense mesoscale eddies and their
interactions with the unstable Algerian Current. The Balearic Basin i
s a transition region between these two different dynamic regimes. It
includes the Catalan Sea, located between the Balearic Islands and the
Iberian peninsula, and the wide Gulf of Valencia in the south of this
sea. Some new ideas about the surface circulation variability have be
en inferred from a series of NOAA satellite advanced very high resolut
ion radiometer images, taken mainly from the autumn-winter period duri
ng 1981-1988, and also from various in situ data. The Northern Current
, which flows southward along the Iberian peninsula slope, is covered
in summer by a warm surface layer spreading over the whole Catalan Sea
. This local warming creates one of the most intense thermal fronts in
the western Mediterranean, the Pyrenees Front. Near the Balearic Isla
nds, the flow through the sills of recent Atlantic water, partially de
flected by anticyclonic eddies from the Algerian Current, creates the
Balearic Front and contributes to its mesoscale variability. This vari
ability appears to be much more intense than previously described. The
Balearic Front is clearly recognized as the westward continuation of
the North Balearic Front, already defined in the open sea as the north
ern limit of the recent Atlantic water reservoir. Finally, the Gulf of
Valencia is frequently influenced by water entering from the Algerian
Basin, which appears to be important in the disruption of the Norther
n Current and the formation of the Balearic Current, the geostrophic f
low associated with the Balearic Front.