Monitoring Atlantic overturning circulation and transport variability with GRACE-type ocean bottom pressure observations – a sensitivity study

The Atlantic Meridional Overturning Circulation (AMOC) is a key mechanism for large-scale northward heat transport and thus plays an important role for global climate. Relatively warm water is transported northward in the upper layers of the North Atlantic Ocean and, after cooling at subpolar latitu...

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Bibliographic Details
Main Authors: K. Bentel, F. W. Landerer, C. Boening
Format: Article
Language:English
Published: Copernicus Publications 2015-12-01
Series:Ocean Science
Online Access:http://www.ocean-sci.net/11/953/2015/os-11-953-2015.pdf