Preserving the coupled atmosphere–ocean feedback in initializations of decadal climate predictions

On interannual to decadal time scales, memory in the Earth's climate system resides to a large extent in the slowly varying heat content of the ocean, which responds to fast atmospheric variability and in turn sets the frame for large-scale atmospheric circulation patterns. This large-scale cou...

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Published in:WIREs Climate Change
Main Authors: Brune, Sebastian, Baehr, Johanna
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.1002/wcc.637
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9369
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spelling ftsubggeo:oai:e-docs.geo-leo.de:11858/9369 2023-05-15T17:34:26+02:00 Preserving the coupled atmosphere–ocean feedback in initializations of decadal climate predictions Brune, Sebastian Baehr, Johanna 2020 https://doi.org/10.1002/wcc.637 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9369 eng eng doi:10.1002/wcc.637 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9369 This is an open access article under the terms of the Creative Commons Attribution-NonCommercial License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited and is not used for commercial purposes. CC-BY-NC ddc:551.6 coupled data assimilation decadal climate prediction earth system model large-scale atmosphere-ocean feedback model-consistent initialization doc-type:article 2020 ftsubggeo https://doi.org/10.1002/wcc.637 2022-11-09T06:51:40Z On interannual to decadal time scales, memory in the Earth's climate system resides to a large extent in the slowly varying heat content of the ocean, which responds to fast atmospheric variability and in turn sets the frame for large-scale atmospheric circulation patterns. This large-scale coupled atmosphere–ocean feedback is generally well represented in today's Earth system models. This may fundamentally change when data assimilation is used to bring such models close to an observed state to initialize interannual to decadal climate predictions. Here, we review how the large-scale coupled atmosphere–ocean feedback is preserved in common approaches to construct such initial conditions, with the focus on the initialized ocean state. In a set of decadal prediction experiments, ranging from an initialization of atmospheric variability only to full-field nudging of both atmosphere and ocean, we evaluate the variability and predictability of the Atlantic meridional overturning circulation, of the Atlantic multidecadal variability and North Atlantic subpolar gyre sea surface temperatures. We argue that the quality of initial conditions for decadal predictions should not purely be assessed by their closeness to observations, but also by the closeness of their respective predictions to observations. This prediction quality may depend on the representation of the simulated large-scale atmosphere–ocean feedback. This article is categorized under: Climate Models and Modeling > Knowledge Generation with Models Article in Journal/Newspaper North Atlantic GEO-LEOe-docs (FID GEO) WIREs Climate Change 11 3
institution Open Polar
collection GEO-LEOe-docs (FID GEO)
op_collection_id ftsubggeo
language English
topic ddc:551.6
coupled data assimilation
decadal climate prediction
earth system model
large-scale atmosphere-ocean feedback
model-consistent initialization
spellingShingle ddc:551.6
coupled data assimilation
decadal climate prediction
earth system model
large-scale atmosphere-ocean feedback
model-consistent initialization
Brune, Sebastian
Baehr, Johanna
Preserving the coupled atmosphere–ocean feedback in initializations of decadal climate predictions
topic_facet ddc:551.6
coupled data assimilation
decadal climate prediction
earth system model
large-scale atmosphere-ocean feedback
model-consistent initialization
description On interannual to decadal time scales, memory in the Earth's climate system resides to a large extent in the slowly varying heat content of the ocean, which responds to fast atmospheric variability and in turn sets the frame for large-scale atmospheric circulation patterns. This large-scale coupled atmosphere–ocean feedback is generally well represented in today's Earth system models. This may fundamentally change when data assimilation is used to bring such models close to an observed state to initialize interannual to decadal climate predictions. Here, we review how the large-scale coupled atmosphere–ocean feedback is preserved in common approaches to construct such initial conditions, with the focus on the initialized ocean state. In a set of decadal prediction experiments, ranging from an initialization of atmospheric variability only to full-field nudging of both atmosphere and ocean, we evaluate the variability and predictability of the Atlantic meridional overturning circulation, of the Atlantic multidecadal variability and North Atlantic subpolar gyre sea surface temperatures. We argue that the quality of initial conditions for decadal predictions should not purely be assessed by their closeness to observations, but also by the closeness of their respective predictions to observations. This prediction quality may depend on the representation of the simulated large-scale atmosphere–ocean feedback. This article is categorized under: Climate Models and Modeling > Knowledge Generation with Models
format Article in Journal/Newspaper
author Brune, Sebastian
Baehr, Johanna
author_facet Brune, Sebastian
Baehr, Johanna
author_sort Brune, Sebastian
title Preserving the coupled atmosphere–ocean feedback in initializations of decadal climate predictions
title_short Preserving the coupled atmosphere–ocean feedback in initializations of decadal climate predictions
title_full Preserving the coupled atmosphere–ocean feedback in initializations of decadal climate predictions
title_fullStr Preserving the coupled atmosphere–ocean feedback in initializations of decadal climate predictions
title_full_unstemmed Preserving the coupled atmosphere–ocean feedback in initializations of decadal climate predictions
title_sort preserving the coupled atmosphere–ocean feedback in initializations of decadal climate predictions
publishDate 2020
url https://doi.org/10.1002/wcc.637
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9369
genre North Atlantic
genre_facet North Atlantic
op_relation doi:10.1002/wcc.637
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9369
op_rights This is an open access article under the terms of the Creative Commons Attribution-NonCommercial License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited and is not used for commercial purposes.
op_rightsnorm CC-BY-NC
op_doi https://doi.org/10.1002/wcc.637
container_title WIREs Climate Change
container_volume 11
container_issue 3
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