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Soviet journal of physical oceanography

, Volume 2, Issue 3, pp 233–237 | Cite as

Observation of the anticyclonic eddy formation off the Black Sea coast

  • N. A. Panteleev
  • A. N. Shcherbakov
Brief Notes
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Abstract

An anticyclonic eddy with a horizontal dimension of ∼ 20 km travelling north-westwards at a speed of 10 cm/s has been found during an experiment carried out off the Black Sea coast. Dynamic instability owing to horizontal velocity shear could be the reason for its origin. The eddy's passage favours the development of shear instability and the generation of short-period internal waves.

Keywords

Climate Change Environmental Physic Internal Wave Horizontal Velocity Velocity Shear 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. 1.
    Blatov, A. S., Bulgakov, N. P. and Ivanov, V. A.Variability of Hydrophysical Fields in the Black Sea. Leningrad: Gidrometeoizdat, (1984), 130 p.Google Scholar
  2. 2.
    Lindstrom, E. J., Eblesmeyer, C. C. and Owens, W. B. Structure and origin of a small cyclonic eddy observed during POLYMODE local dynamic experiment.J. Phys. Ocean. (1986)16, 562–570.Google Scholar

Copyright information

© VSP 1991

Authors and Affiliations

  • N. A. Panteleev
  • A. N. Shcherbakov

There are no affiliations available

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