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Mechanisms of Atlantic Meridional Overturning Circulation variability simulated by the NEMO model

We have investigated mechanisms for the Atlantic Meridional Overturning Circulation (AMOC) variability at 26.5° N (other than the Ekman component) that can be related to external forcings, in particular wind variability. Resolution dependence is studied using identical experiments with 1° and 1/4° N...

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Bibliografische gegevens
Hoofdauteurs: V. N. Stepanov, K. Haines
Formaat: Artigo
Taal:Inglês
Gepubliceerd in: Copernicus Publications 2014-07-01
Reeks:Ocean Science
Online toegang:http://www.ocean-sci.net/10/645/2014/os-10-645-2014.pdf
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