exactly to the theoretical value that was calculated at the point of the sampling
(Table 9.1). The differences are due to the nonhomogeneity of the measured current
velocity in different time (month ad year).
Different processing approaches were used: the integrated hodograph and the
Fast Fourier Transform. In the western continental Black Sea shelf are showed the
presence of periodic motions: long waves (periods of hours) and short waves
Fig. 9.2 Development of the inertial current vector during sampling
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M.-E. Mihailov