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


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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.

作者简介

T. Demidova

Shirshov Institute of Oceanology

Email: vneiman2007@yandex.ru
俄罗斯联邦, Moscow, 117218

E. Morozov

Shirshov Institute of Oceanology

Email: vneiman2007@yandex.ru
俄罗斯联邦, Moscow, 117218

V. Neiman

Shirshov Institute of Oceanology

编辑信件的主要联系方式.
Email: vneiman2007@yandex.ru
俄罗斯联邦, Moscow, 117218

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