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...

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Main Authors: Persechino, A., /Mignot, Juliette, Swingedouw, D., Labetoulle, S., Guilyardi, E.
Format: Text
Language:English
Published: 2013
Subjects:
Online Access:https://www.documentation.ird.fr/hor/fdi:010060873
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spelling ftird:oai:ird.fr:fdi:010060873 2024-09-15T18:20:30+00:00 Decadal predictability of the Atlantic meridional overturning circulation and climate in the IPSL-CM5A-LR model Presentation and analysis of the IPSL and CNRM climate models used in CMIP5 Persechino, A. /Mignot, Juliette Swingedouw, D. Labetoulle, S. Guilyardi, E. OCEAN ATLANTIQUE ZONE MERIDIONALE 2013 https://www.documentation.ird.fr/hor/fdi:010060873 EN eng https://www.documentation.ird.fr/hor/fdi:010060873 oai:ird.fr:fdi:010060873 Persechino A., Mignot Juliette, Swingedouw D., Labetoulle S., Guilyardi E. Decadal predictability of the Atlantic meridional overturning circulation and climate in the IPSL-CM5A-LR model. In : . Presentation and analysis of the IPSL and CNRM climate models used in CMIP5 2013, 40 (9-10), p. 2359-2380 Decadal climate predictability Atlantic meridional overturning circulation Diagnostic and prognostic potential predictability Ocean and climate dynamics text 2013 ftird 2024-08-15T05:57:42Z 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. Text Nordic Seas North Atlantic IRD (Institute de recherche pour le développement): Horizon
institution Open Polar
collection IRD (Institute de recherche pour le développement): Horizon
op_collection_id ftird
language English
topic Decadal climate predictability
Atlantic meridional overturning circulation
Diagnostic and prognostic potential predictability
Ocean and climate dynamics
spellingShingle Decadal climate predictability
Atlantic meridional overturning circulation
Diagnostic and prognostic potential predictability
Ocean and climate dynamics
Persechino, A.
/Mignot, Juliette
Swingedouw, D.
Labetoulle, S.
Guilyardi, E.
Decadal predictability of the Atlantic meridional overturning circulation and climate in the IPSL-CM5A-LR model
topic_facet Decadal climate predictability
Atlantic meridional overturning circulation
Diagnostic and prognostic potential predictability
Ocean and climate dynamics
description 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.
format Text
author Persechino, A.
/Mignot, Juliette
Swingedouw, D.
Labetoulle, S.
Guilyardi, E.
author_facet Persechino, A.
/Mignot, Juliette
Swingedouw, D.
Labetoulle, S.
Guilyardi, E.
author_sort Persechino, A.
title Decadal predictability of the Atlantic meridional overturning circulation and climate in the IPSL-CM5A-LR model
title_short Decadal predictability of the Atlantic meridional overturning circulation and climate in the IPSL-CM5A-LR model
title_full Decadal predictability of the Atlantic meridional overturning circulation and climate in the IPSL-CM5A-LR model
title_fullStr Decadal predictability of the Atlantic meridional overturning circulation and climate in the IPSL-CM5A-LR model
title_full_unstemmed Decadal predictability of the Atlantic meridional overturning circulation and climate in the IPSL-CM5A-LR model
title_sort decadal predictability of the atlantic meridional overturning circulation and climate in the ipsl-cm5a-lr model
publishDate 2013
url https://www.documentation.ird.fr/hor/fdi:010060873
op_coverage OCEAN ATLANTIQUE
ZONE MERIDIONALE
genre Nordic Seas
North Atlantic
genre_facet Nordic Seas
North Atlantic
op_relation https://www.documentation.ird.fr/hor/fdi:010060873
oai:ird.fr:fdi:010060873
Persechino A., Mignot Juliette, Swingedouw D., Labetoulle S., Guilyardi E. Decadal predictability of the Atlantic meridional overturning circulation and climate in the IPSL-CM5A-LR model. In : . Presentation and analysis of the IPSL and CNRM climate models used in CMIP5 2013, 40 (9-10), p. 2359-2380
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