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The Lomonosov Equatorial Undercurrent according to Data Measured with a Shipborne Profiler, 2014–2017


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Abstract

The velocity and structure of the Lomonosov Equatorial Undercurrent of the Atlantic Ocean are determined based on the data measured with a shipborne acoustic profiler from 2014 to 2017. The seasonal variability of this flow is estimated, and the cases of its outcropping to the surface in the spring of the Northern Hemisphere are revealed.

About the authors

T. A. Demidova

Shirshov Institute of Oceanology

Email: vneiman2007@yandex.ru
Russian Federation, Moscow, 117218

E. G. Morozov

Shirshov Institute of Oceanology

Email: vneiman2007@yandex.ru
Russian Federation, Moscow, 117218

V. G. Neiman

Shirshov Institute of Oceanology

Author for correspondence.
Email: vneiman2007@yandex.ru
Russian Federation, Moscow, 117218

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