the Romanian shelf (44 10
0 N, 29 22
0 E) and offshore Mamaia Bay (44
12
0 N–
28
20
0 E).
The inertial oscillations are a transient motion developed by Coriolis force and
inertia which results from a dynamic adjustment (such as surface wind stress). For
the Romanian shelf was calculated the inertial period which range from 16.5 to
17.5 h. The extracted inertial periodic component does not always correspond
Fig. 9.1 Long period inertial currents charts, on the western Black Sea
9 Inertial Currents in Western Continental Black Sea Shelf
147
0 N, 29 22
0 E) and offshore Mamaia Bay (44
12
0 N–
28
20
0 E).
The inertial oscillations are a transient motion developed by Coriolis force and
inertia which results from a dynamic adjustment (such as surface wind stress). For
the Romanian shelf was calculated the inertial period which range from 16.5 to
17.5 h. The extracted inertial periodic component does not always correspond
Fig. 9.1 Long period inertial currents charts, on the western Black Sea
9 Inertial Currents in Western Continental Black Sea Shelf
147