North Atlantic climate model bias influence on multiyear predictability

The influences of North Atlantic biases on multiyear predictability of unforced surface air temperature (SAT) variability are examined in the Kiel Climate Model (KCM). By employing a freshwater flux correction over the North Atlantic to the model, which strongly alleviates both North Atlantic sea su...

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Published in:Earth and Planetary Science Letters
Main Authors: Wu, Yanling, Park, Taewook, Park, Wonsun, Latif, Mojib
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2018
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/40275/
https://oceanrep.geomar.de/id/eprint/40275/1/1-s2.0-S0012821X1730571X-main.pdf
https://oceanrep.geomar.de/id/eprint/40275/2/1-s2.0-S0012821X1730571X-mmc1.doc
https://doi.org/10.1016/j.epsl.2017.10.012
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spelling ftoceanrep:oai:oceanrep.geomar.de:40275 2023-05-15T17:25:30+02:00 North Atlantic climate model bias influence on multiyear predictability Wu, Yanling Park, Taewook Park, Wonsun Latif, Mojib 2018-01-01 text https://oceanrep.geomar.de/id/eprint/40275/ https://oceanrep.geomar.de/id/eprint/40275/1/1-s2.0-S0012821X1730571X-main.pdf https://oceanrep.geomar.de/id/eprint/40275/2/1-s2.0-S0012821X1730571X-mmc1.doc https://doi.org/10.1016/j.epsl.2017.10.012 en eng Elsevier https://oceanrep.geomar.de/id/eprint/40275/1/1-s2.0-S0012821X1730571X-main.pdf https://oceanrep.geomar.de/id/eprint/40275/2/1-s2.0-S0012821X1730571X-mmc1.doc Wu, Y., Park, T., Park, W. and Latif, M. (2018) North Atlantic climate model bias influence on multiyear predictability. Earth and Planetary Science Letters, 481 . pp. 171-176. DOI 10.1016/j.epsl.2017.10.012 <https://doi.org/10.1016/j.epsl.2017.10.012>. doi:10.1016/j.epsl.2017.10.012 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2018 ftoceanrep https://doi.org/10.1016/j.epsl.2017.10.012 2023-04-07T15:36:32Z The influences of North Atlantic biases on multiyear predictability of unforced surface air temperature (SAT) variability are examined in the Kiel Climate Model (KCM). By employing a freshwater flux correction over the North Atlantic to the model, which strongly alleviates both North Atlantic sea surface salinity (SSS) and sea surface temperature (SST) biases, the freshwater flux-corrected integration depicts significantly enhanced multiyear SAT predictability in the North Atlantic sector in comparison to the uncorrected one. The enhanced SAT predictability in the corrected integration is due to a stronger and more variable Atlantic Meridional Overturning Circulation (AMOC) and its enhanced influence on North Atlantic SST. Results obtained from preindustrial control integrations of models participating in the Coupled Model Intercomparison Project Phase 5 (CMIP5) support the findings obtained from the KCM: models with large North Atlantic biases tend to have a weak AMOC influence on SAT and exhibit a smaller SAT predictability over the North Atlantic sector. Article in Journal/Newspaper North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Earth and Planetary Science Letters 481 171 176
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description The influences of North Atlantic biases on multiyear predictability of unforced surface air temperature (SAT) variability are examined in the Kiel Climate Model (KCM). By employing a freshwater flux correction over the North Atlantic to the model, which strongly alleviates both North Atlantic sea surface salinity (SSS) and sea surface temperature (SST) biases, the freshwater flux-corrected integration depicts significantly enhanced multiyear SAT predictability in the North Atlantic sector in comparison to the uncorrected one. The enhanced SAT predictability in the corrected integration is due to a stronger and more variable Atlantic Meridional Overturning Circulation (AMOC) and its enhanced influence on North Atlantic SST. Results obtained from preindustrial control integrations of models participating in the Coupled Model Intercomparison Project Phase 5 (CMIP5) support the findings obtained from the KCM: models with large North Atlantic biases tend to have a weak AMOC influence on SAT and exhibit a smaller SAT predictability over the North Atlantic sector.
format Article in Journal/Newspaper
author Wu, Yanling
Park, Taewook
Park, Wonsun
Latif, Mojib
spellingShingle Wu, Yanling
Park, Taewook
Park, Wonsun
Latif, Mojib
North Atlantic climate model bias influence on multiyear predictability
author_facet Wu, Yanling
Park, Taewook
Park, Wonsun
Latif, Mojib
author_sort Wu, Yanling
title North Atlantic climate model bias influence on multiyear predictability
title_short North Atlantic climate model bias influence on multiyear predictability
title_full North Atlantic climate model bias influence on multiyear predictability
title_fullStr North Atlantic climate model bias influence on multiyear predictability
title_full_unstemmed North Atlantic climate model bias influence on multiyear predictability
title_sort north atlantic climate model bias influence on multiyear predictability
publisher Elsevier
publishDate 2018
url https://oceanrep.geomar.de/id/eprint/40275/
https://oceanrep.geomar.de/id/eprint/40275/1/1-s2.0-S0012821X1730571X-main.pdf
https://oceanrep.geomar.de/id/eprint/40275/2/1-s2.0-S0012821X1730571X-mmc1.doc
https://doi.org/10.1016/j.epsl.2017.10.012
genre North Atlantic
genre_facet North Atlantic
op_relation https://oceanrep.geomar.de/id/eprint/40275/1/1-s2.0-S0012821X1730571X-main.pdf
https://oceanrep.geomar.de/id/eprint/40275/2/1-s2.0-S0012821X1730571X-mmc1.doc
Wu, Y., Park, T., Park, W. and Latif, M. (2018) North Atlantic climate model bias influence on multiyear predictability. Earth and Planetary Science Letters, 481 . pp. 171-176. DOI 10.1016/j.epsl.2017.10.012 <https://doi.org/10.1016/j.epsl.2017.10.012>.
doi:10.1016/j.epsl.2017.10.012
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1016/j.epsl.2017.10.012
container_title Earth and Planetary Science Letters
container_volume 481
container_start_page 171
op_container_end_page 176
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