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OCEANIC CONVECTION AND STRATIFICATION IN THE NORTHERN ATLANTIC AS OB SERVED IN WINTER 2013/14

Abstract

Spatial characteristics of oceanic convection in the North Atlantic Subpolar Gyre in winter 2013/14 are investigated basing on the analysis of Argo float data. Domains of the most intense convective mixing are identified by quantifying and mapping the water column vertical stratification. The areas of the Subpolar Mode Water formation are found along the Irminger Current, namely over the northwestern slope of the Reykjanes Ridge and in the vicinity of the Denmark Strait. The location of convection domains and the spatial changes of mixed layer properties in these domains are in a good agreement with a contemporary concept stating the localized formation of the mode waters along each of the individual branches of the North Atlantic Current and the increasing density of the mode waters in the northward direction. The main role in the formation of the Labrador Sea Water belonged to the convection zone in the Labrador Sea, where the mixing depth reached 1750 m for the first time over the past six years. The relatively cold and fresh intermediate waters, matching the Labrador Sea Water in their properties, were also formed in the domain to the south of the Cape Farewell and in the southern part of the Irminger Sea.

About the Authors

A. S. Falina
Shirshov Institute of Oceanology of the Russian Academy of Sciences.
Russian Federation
Laboratory of Hydrological Processes, Senior Research Scientist, PhD in Geography.


A. A. Sarafanov
Shirshov Institute of Oceanology of the Russian Academy of Sciences.
Russian Federation
Laboratory of Hydrological Processes, Senior Research Scientist, D.Sc. in Geography.


S. A. Dobrolyubov
Lomonosov Moscow State University.
Russian Federation
Faculty of Geography, Dean of the Faculty, Professor, D.Sc. in Geography.


V. S. Zapotylko
Shirshov Institute of Oceanology of the Russian Academy of Sciences.
Russian Federation
Department of Scientific Expeditions and Fleet, main expert.


S. V. Gladyshev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Russian Federation
Department of Scientific Expeditions and Fleet, Deputy Head of the Department.


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Review

For citations:


Falina A.S., Sarafanov A.A., Dobrolyubov S.A., Zapotylko V.S., Gladyshev S.V. OCEANIC CONVECTION AND STRATIFICATION IN THE NORTHERN ATLANTIC AS OB SERVED IN WINTER 2013/14. Vestnik Moskovskogo universiteta. Seriya 5, Geografiya. 2017;(4):45-54. (In Russ.)

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ISSN 0579-9414 (Print)