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Structure and variability of current and water temperature fields near the Mascarene Ridge

  • Experimental and Field Research
  • Published:
Soviet journal of physical oceanography

Abstract

An anticyclonic mesoscale eddy is found using the current and temperature data obtained at six moorings near the eastern foot of the Mascarene Ridge (Southern Hemisphere). Its spatial parameters radius, depth of penetration, and direction of the vertical axis tilt are given. The volume of water transported by the eddy across its radial section is calculated. Numerical characteristics of the spatial-temporal variability of the current and temperature field in the eddy are obtained. The relative contributions of the variability of mesoscale, tidal and inertial, and high-frequency oscillations are estimated.

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References

  1. Atlas of the Oceans. The Atlantic and Indian Oceans. Moscow: Hydrography and Navigation Department, Defence Ministry of the USSR (1977), 306 p.

  2. Burenkov, V. I. and Vasil'kov, A. P. Study of characteristics of internal waves in the upper thermocline near the Mascarene Ridge.Okeanologia (1987)27, 191–196.

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Translated by Mikhail M. Trufanov.

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Titov, V.B. Structure and variability of current and water temperature fields near the Mascarene Ridge. Soviet Journal of Physical Oceanography 1, 461–468 (1990). https://doi.org/10.1007/BF02197000

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  • DOI: https://doi.org/10.1007/BF02197000

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