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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8588

Authors: Pohlmann, H.*
Smith, D. M.*
Balmaseda, M. A.*
Keenlyside, N. S.*
Masina, S.*
Matei, D.*
Muller, W. A.*
Rogel, P.*
Title: Predictability of the mid-latitude Atlantic meridional overturning circulation in a multi-model system
Title of journal: Climate dynamics
Series/Report no.: /41 (2013)
Publisher: Springer Verlag GMBH Germany
Issue Date: 2013
DOI: 10.1007/s00382-013-1663-6
Keywords: Decadal prediction 􏰁 Atlantic MOC 􏰁 Predictability 􏰁 Multi-model comparison
Abstract: Assessing the skill of the Atlantic meridional overturning circulation (AMOC) in decadal hindcasts (i.e. retrospective predictions) is hampered by a lack of obser- vations for verification. Models are therefore needed to reconstruct the historical AMOC variability. Here we show that ten recent oceanic syntheses provide a common signal of AMOC variability at 45°N, with an increase from the 1960s to the mid-1990s and a decrease thereafter although they disagree on the exact magnitude. This signal corre- lates with observed key processes such as the North Atlantic Oscillation, sub-polar gyre strength, Atlantic sea surface temperature dipole, and Labrador Sea convection that are thought to be related to the AMOC. Furthermore, we find potential predictability of the mid-latitude AMOC for the first 3–6 year means when we validate decadal hindcasts for the past 50 years against the multi-model signal. However, this predictability is not found in models driven only by external radiative changes, demonstrating the need for initialization of decadal climate predictions.
Appears in Collections:01.01.02. Climate
03.01.03. Global climate models
03.03.03. Interannual-to-decadal ocean variability
Papers Published / Papers in press

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