Wind induced oscillator dynamics in the Black Sea revealed by Lagrangian drifters

Physics

Scientific paper

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Oceanography: General: Marginal And Semi-Enclosed Seas, Oceanography: Physical: Currents, Oceanography: Physical: Hydrography And Tracers

Scientific paper

Lagrangian drifter observations of the Black Sea circulation between 2002 and 2003 show six transitions between two meta-stable states representing single gyre structures centered in either the western or eastern sub-basin of the Black Sea, respectively. The major mechanisms driving such an oscillator dynamics are Ekman pumping for the eastern sub-basin, and most likely a resonance excitation for the western sub-basin. The sea strongly amplifies the wind responses of 120-day periodicity. Data analysis demonstrates that two-gyre structure (``Knipovich spectacles'') was a transient between the states. Residence time for the sea to occupy either state is mainly determined by the instability of the gyres, wind variability and, probably, variations in the pycnocline. This behavior is a manifestation of a bimodal dynamical regime which affects the long-term (climatic), large-scale transport and mixing of bio-geochemical substances.

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