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Decadal predictability of the Atlantic meridional overturning circulation and climate in the IPSL-CM5A-LR model

Decadal predictability of the Atlantic meridional overturning circulation and climate in the IPSL-CM5A-LR model
Decadal predictability of the Atlantic meridional overturning circulation and climate in the IPSL-CM5A-LR model
This study explores the decadal potential predictability of the Atlantic Meridional Overturning Circulation (AMOC) as represented in the IPSL-CM5A-LR model, along with the predictability of associated oceanic and atmospheric fields. Using a 1000-year control run, we analyze the prognostic potential predictability (PPP) of the AMOC through ensembles of simulations with perturbed initial conditions. Based on a measure of the ensemble spread, the modelled AMOC has an average predictive skill of 8 years, with some degree of dependence on the AMOC initial state. Diagnostic potential predictability of surface temperature and precipitation is also identified in the control run and compared to the PPP. Both approaches clearly bring out the same regions exhibiting the highest predictive skill. Generally, surface temperature has the highest skill up to 2 decades in the far North Atlantic ocean. There are also weak signals over a few oceanic areas in the tropics and subtropics. Predictability over land is restricted to the coastal areas bordering oceanic predictable regions. Potential predictability at interannual and longer timescales is largely absent for precipitation in spite of weak signals identified mainly in the Nordic Seas. Regions of weak signals show some dependence on AMOC initial state. All the identified regions are closely linked to decadal AMOC fluctuations suggesting that the potential predictability of climate arises from the mechanisms controlling these fluctuations. Evidence for dependence on AMOC initial state also suggests that studying skills from case studies may prove more useful to understand predictability mechanisms than computing average skill from numerous start dates.
Decadal climate predictability, Atlantic meridional overturning circulation, Diagnostic and prognostic potential predictability, Ocean and climate dynamics
0930-7575
2359-2380
Persechino, A.
516687cb-440c-4cc3-91e9-21233b28ae04
Mignot, J.
979e956d-18e7-4d4b-8158-3b9362187ed4
Swingedouw, D.
27dd68d4-2212-4f5c-a65f-eac60055eb24
Labetoulle, S.
fed2bd7a-cfe1-452d-bcf4-cb56ed7eb36e
Guilyardi, E.
d8e3cd51-7353-401c-994a-7bee46dc4b6b
Persechino, A.
516687cb-440c-4cc3-91e9-21233b28ae04
Mignot, J.
979e956d-18e7-4d4b-8158-3b9362187ed4
Swingedouw, D.
27dd68d4-2212-4f5c-a65f-eac60055eb24
Labetoulle, S.
fed2bd7a-cfe1-452d-bcf4-cb56ed7eb36e
Guilyardi, E.
d8e3cd51-7353-401c-994a-7bee46dc4b6b

Persechino, A., Mignot, J., Swingedouw, D., Labetoulle, S. and Guilyardi, E. (2013) Decadal predictability of the Atlantic meridional overturning circulation and climate in the IPSL-CM5A-LR model. Climate Dynamics, 40 (9-10), 2359-2380. (doi:10.1007/s00382-012-1466-1).

Record type: Article

Abstract

This study explores the decadal potential predictability of the Atlantic Meridional Overturning Circulation (AMOC) as represented in the IPSL-CM5A-LR model, along with the predictability of associated oceanic and atmospheric fields. Using a 1000-year control run, we analyze the prognostic potential predictability (PPP) of the AMOC through ensembles of simulations with perturbed initial conditions. Based on a measure of the ensemble spread, the modelled AMOC has an average predictive skill of 8 years, with some degree of dependence on the AMOC initial state. Diagnostic potential predictability of surface temperature and precipitation is also identified in the control run and compared to the PPP. Both approaches clearly bring out the same regions exhibiting the highest predictive skill. Generally, surface temperature has the highest skill up to 2 decades in the far North Atlantic ocean. There are also weak signals over a few oceanic areas in the tropics and subtropics. Predictability over land is restricted to the coastal areas bordering oceanic predictable regions. Potential predictability at interannual and longer timescales is largely absent for precipitation in spite of weak signals identified mainly in the Nordic Seas. Regions of weak signals show some dependence on AMOC initial state. All the identified regions are closely linked to decadal AMOC fluctuations suggesting that the potential predictability of climate arises from the mechanisms controlling these fluctuations. Evidence for dependence on AMOC initial state also suggests that studying skills from case studies may prove more useful to understand predictability mechanisms than computing average skill from numerous start dates.

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More information

Published date: May 2013
Keywords: Decadal climate predictability, Atlantic meridional overturning circulation, Diagnostic and prognostic potential predictability, Ocean and climate dynamics
Organisations: Physical Oceanography

Identifiers

Local EPrints ID: 353518
URI: http://eprints.soton.ac.uk/id/eprint/353518
ISSN: 0930-7575
PURE UUID: 150eea90-842f-4c92-a301-ec2e40c306ab

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Date deposited: 07 Jun 2013 11:00
Last modified: 14 Mar 2024 14:06

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Contributors

Author: A. Persechino
Author: J. Mignot
Author: D. Swingedouw
Author: S. Labetoulle
Author: E. Guilyardi

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