Water masses characteristics of the northern Aegean Sea were investiga
ted based upon historical Nansen cast data. Cyclonic surface circulati
on carries Black Sea water towards the west, and it then follows a sou
th-south-westerly route. Less saline surface water of the Black Sea or
igin was observed in the western part of the area. The source of inter
mediate water was identified by slightly elevated salinity located in
the south and south-eastern parts of the region. Intermediate water tr
ansport towards the north and north-west. may possibly compensate for
south-bound surface water transport. Deep water with high oxygen conte
nt is formed in the Kavala, Kassandra and Saros Gulfs of the northern
basin. (C) 1995 Academic Press Limited