A global hybrid coupled model based on Atmosphere-SST feedbacks

A global hybrid coupled model is developed, with the aim of studying the effects of ocean-atmosphere feedbacks on the stability of the Atlantic meridional overturning circulation. The model includes a global ocean general circulation model and a statistical atmosphere model. The statistical atmosphe...

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Main Authors: Cimatoribus, Andrea A., Drijfhout, Sybren S., Dijkstra, Henk A.
Format: Text
Language:unknown
Published: arXiv 2011
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.1101.4096
https://arxiv.org/abs/1101.4096
id ftdatacite:10.48550/arxiv.1101.4096
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spelling ftdatacite:10.48550/arxiv.1101.4096 2023-05-15T17:33:14+02:00 A global hybrid coupled model based on Atmosphere-SST feedbacks Cimatoribus, Andrea A. Drijfhout, Sybren S. Dijkstra, Henk A. 2011 https://dx.doi.org/10.48550/arxiv.1101.4096 https://arxiv.org/abs/1101.4096 unknown arXiv https://dx.doi.org/10.1007/s00382-011-1094-1 arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Atmospheric and Oceanic Physics physics.ao-ph Chaotic Dynamics nlin.CD FOS Physical sciences article-journal Article ScholarlyArticle Text 2011 ftdatacite https://doi.org/10.48550/arxiv.1101.4096 https://doi.org/10.1007/s00382-011-1094-1 2022-04-01T14:34:50Z A global hybrid coupled model is developed, with the aim of studying the effects of ocean-atmosphere feedbacks on the stability of the Atlantic meridional overturning circulation. The model includes a global ocean general circulation model and a statistical atmosphere model. The statistical atmosphere model is based on linear regressions of data from a fully coupled climate model on sea surface temperature both locally and hemispherically averaged, being the footprint of Atlantic meridional overturning variability. It provides dynamic boundary conditions to the ocean model for heat, freshwater and wind-stress. A basic but consistent representation of ocean-atmosphere feedbacks is captured in the hybrid coupled model and it is more than ten times faster than the fully coupled climate model. The hybrid coupled model reaches a steady state with a climate close to the one of the fully coupled climate model, and the two models also have a similar response (collapse) of the Atlantic meridional overturning circulation to a freshwater hosing applied in the northern North Atlantic. : The final publication is available at springerlink.com Text North Atlantic DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Atmospheric and Oceanic Physics physics.ao-ph
Chaotic Dynamics nlin.CD
FOS Physical sciences
spellingShingle Atmospheric and Oceanic Physics physics.ao-ph
Chaotic Dynamics nlin.CD
FOS Physical sciences
Cimatoribus, Andrea A.
Drijfhout, Sybren S.
Dijkstra, Henk A.
A global hybrid coupled model based on Atmosphere-SST feedbacks
topic_facet Atmospheric and Oceanic Physics physics.ao-ph
Chaotic Dynamics nlin.CD
FOS Physical sciences
description A global hybrid coupled model is developed, with the aim of studying the effects of ocean-atmosphere feedbacks on the stability of the Atlantic meridional overturning circulation. The model includes a global ocean general circulation model and a statistical atmosphere model. The statistical atmosphere model is based on linear regressions of data from a fully coupled climate model on sea surface temperature both locally and hemispherically averaged, being the footprint of Atlantic meridional overturning variability. It provides dynamic boundary conditions to the ocean model for heat, freshwater and wind-stress. A basic but consistent representation of ocean-atmosphere feedbacks is captured in the hybrid coupled model and it is more than ten times faster than the fully coupled climate model. The hybrid coupled model reaches a steady state with a climate close to the one of the fully coupled climate model, and the two models also have a similar response (collapse) of the Atlantic meridional overturning circulation to a freshwater hosing applied in the northern North Atlantic. : The final publication is available at springerlink.com
format Text
author Cimatoribus, Andrea A.
Drijfhout, Sybren S.
Dijkstra, Henk A.
author_facet Cimatoribus, Andrea A.
Drijfhout, Sybren S.
Dijkstra, Henk A.
author_sort Cimatoribus, Andrea A.
title A global hybrid coupled model based on Atmosphere-SST feedbacks
title_short A global hybrid coupled model based on Atmosphere-SST feedbacks
title_full A global hybrid coupled model based on Atmosphere-SST feedbacks
title_fullStr A global hybrid coupled model based on Atmosphere-SST feedbacks
title_full_unstemmed A global hybrid coupled model based on Atmosphere-SST feedbacks
title_sort global hybrid coupled model based on atmosphere-sst feedbacks
publisher arXiv
publishDate 2011
url https://dx.doi.org/10.48550/arxiv.1101.4096
https://arxiv.org/abs/1101.4096
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.1007/s00382-011-1094-1
op_rights arXiv.org perpetual, non-exclusive license
http://arxiv.org/licenses/nonexclusive-distrib/1.0/
op_doi https://doi.org/10.48550/arxiv.1101.4096
https://doi.org/10.1007/s00382-011-1094-1
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