(periods 1 h). In the case of inertial with short periods, the rotation of the current
vector of the short period motions has a cyclonic sense of and the periods are tens of
minutes.
Fig. 9.3 The oscillation frequency of long periods inertial currents
9 Inertial Currents in Western Continental Black Sea Shelf
149
vector of the short period motions has a cyclonic sense of and the periods are tens of
minutes.
Fig. 9.3 The oscillation frequency of long periods inertial currents
9 Inertial Currents in Western Continental Black Sea Shelf
149
