We address in this paper the planetary basin modes and their possible impac
t on the circulation of Black Sea. These oscillations could become importan
t in semi-enclosed seas where the horizontal scales are smaller than the ba
rotropic radius of deformation and the baroclinic radius of deformation is
comparable with the basin scales. The physical balances studied here are ba
sed on theoretical results for the Rossby modes in rectangular basins and o
n model simulations carried out with Bryan-Cox ocean model with eddy resolu
tion. Eddies with horizontal scales of 100-200 km spontaneously form and pr
opagate to the west with phase velocity of few kilometers per day. External
mode oscillations dominate the model solution and show close similarity wi
th estimates based on simplistic theoretical models. In the baroclinic ocea
ns these oscillations trigger active baroclinic variability and western pro
pagation, but with strongly modified wave characteristics in comparison to
the barotropic case. The comparisons between simulations and data from surv
eys and altimeters demonstrates that the planetary modes are a dominating f
orm of wave motion in this sea and can explain the westward propagation of
signals in its deep part. It is suggested that the excitation of rotational
modes can be also important for the dispersion of tracers. (C) 1999 Elsevi
er Science B.V. All rights reserved.