Enviar artigo por via de e-mail The North Atlantic Oscillation: A dominant factor in variations of oceanic circulation systems of the Atlantic Ocean
- Autores: Dvoryaninov G.S.1, Kubryakov A.A.1, Sizov A.A.1, Stanichny S.V.1, Shapiro N.B.1
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Afiliações:
- Marine Hydrophysical Institute
- Edição: Volume 466, Nº 1 (2016)
- Páginas: 100-104
- Seção: Geography
- URL: https://ogarev-online.ru/1028-334X/article/view/187990
- DOI: https://doi.org/10.1134/S1028334X16010207
- ID: 187990
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Resumo
On the basis of altimetry data, the dynamics of the interaction between the subtropical anticyclonic (SA) and subpolar cyclonic (SC) gyres of the North Atlantic is considered. It is shown that the westerlies in the lower troposphere represented by the North Atlantic Oscillation (NAO) index are the main factor responsible for the dynamics of the gyres, which controls the inflow of warm Atlantic water into the Polar basin.
Sobre autores
G. Dvoryaninov
Marine Hydrophysical Institute
Email: Sizov_anatoliy@mail.ru
Rússia, Sevastopol
A. Kubryakov
Marine Hydrophysical Institute
Email: Sizov_anatoliy@mail.ru
Rússia, Sevastopol
A. Sizov
Marine Hydrophysical Institute
Autor responsável pela correspondência
Email: Sizov_anatoliy@mail.ru
Rússia, Sevastopol
S. Stanichny
Marine Hydrophysical Institute
Email: Sizov_anatoliy@mail.ru
Rússia, Sevastopol
N. Shapiro
Marine Hydrophysical Institute
Email: Sizov_anatoliy@mail.ru
Rússia, Sevastopol
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