NAO predictability from external forcing in the late 20th century

Abstract The North Atlantic Oscillation (NAO) is predictable in climate models at near-decadal timescales. Predictive skill derives from ocean initialization, which can capture variability internal to the climate system, and from external radiative forcing. Herein, we show that predictive skill for...

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Published in:npj Climate and Atmospheric Science
Main Authors: Jeremy M. Klavans, Mark A. Cane, Amy C. Clement, Lisa N. Murphy
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2021
Subjects:
Online Access:https://doi.org/10.1038/s41612-021-00177-8
https://doaj.org/article/96e2c3bf8c0f4d6787701274dcf87ec5
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spelling ftdoajarticles:oai:doaj.org/article:96e2c3bf8c0f4d6787701274dcf87ec5 2023-05-15T17:28:32+02:00 NAO predictability from external forcing in the late 20th century Jeremy M. Klavans Mark A. Cane Amy C. Clement Lisa N. Murphy 2021-03-01T00:00:00Z https://doi.org/10.1038/s41612-021-00177-8 https://doaj.org/article/96e2c3bf8c0f4d6787701274dcf87ec5 EN eng Nature Portfolio https://doi.org/10.1038/s41612-021-00177-8 https://doaj.org/toc/2397-3722 doi:10.1038/s41612-021-00177-8 2397-3722 https://doaj.org/article/96e2c3bf8c0f4d6787701274dcf87ec5 npj Climate and Atmospheric Science, Vol 4, Iss 1, Pp 1-8 (2021) Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2021 ftdoajarticles https://doi.org/10.1038/s41612-021-00177-8 2022-12-31T05:21:22Z Abstract The North Atlantic Oscillation (NAO) is predictable in climate models at near-decadal timescales. Predictive skill derives from ocean initialization, which can capture variability internal to the climate system, and from external radiative forcing. Herein, we show that predictive skill for the NAO in a very large uninitialized multi-model ensemble is commensurate with previously reported skill from a state-of-the-art initialized prediction system. The uninitialized ensemble and initialized prediction system produce similar levels of skill for northern European precipitation and North Atlantic SSTs. Identifying these predictable components becomes possible in a very large ensemble, confirming the erroneously low signal-to-noise ratio previously identified in both initialized and uninitialized climate models. Though the results here imply that external radiative forcing is a major source of predictive skill for the NAO, they also indicate that ocean initialization may be important for particular NAO events (the mid-1990s strong positive NAO), and, as previously suggested, in certain ocean regions such as the subpolar North Atlantic ocean. Overall, we suggest that improving climate models’ response to external radiative forcing may help resolve the known signal-to-noise error in climate models. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Directory of Open Access Journals: DOAJ Articles npj Climate and Atmospheric Science 4 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Jeremy M. Klavans
Mark A. Cane
Amy C. Clement
Lisa N. Murphy
NAO predictability from external forcing in the late 20th century
topic_facet Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Abstract The North Atlantic Oscillation (NAO) is predictable in climate models at near-decadal timescales. Predictive skill derives from ocean initialization, which can capture variability internal to the climate system, and from external radiative forcing. Herein, we show that predictive skill for the NAO in a very large uninitialized multi-model ensemble is commensurate with previously reported skill from a state-of-the-art initialized prediction system. The uninitialized ensemble and initialized prediction system produce similar levels of skill for northern European precipitation and North Atlantic SSTs. Identifying these predictable components becomes possible in a very large ensemble, confirming the erroneously low signal-to-noise ratio previously identified in both initialized and uninitialized climate models. Though the results here imply that external radiative forcing is a major source of predictive skill for the NAO, they also indicate that ocean initialization may be important for particular NAO events (the mid-1990s strong positive NAO), and, as previously suggested, in certain ocean regions such as the subpolar North Atlantic ocean. Overall, we suggest that improving climate models’ response to external radiative forcing may help resolve the known signal-to-noise error in climate models.
format Article in Journal/Newspaper
author Jeremy M. Klavans
Mark A. Cane
Amy C. Clement
Lisa N. Murphy
author_facet Jeremy M. Klavans
Mark A. Cane
Amy C. Clement
Lisa N. Murphy
author_sort Jeremy M. Klavans
title NAO predictability from external forcing in the late 20th century
title_short NAO predictability from external forcing in the late 20th century
title_full NAO predictability from external forcing in the late 20th century
title_fullStr NAO predictability from external forcing in the late 20th century
title_full_unstemmed NAO predictability from external forcing in the late 20th century
title_sort nao predictability from external forcing in the late 20th century
publisher Nature Portfolio
publishDate 2021
url https://doi.org/10.1038/s41612-021-00177-8
https://doaj.org/article/96e2c3bf8c0f4d6787701274dcf87ec5
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source npj Climate and Atmospheric Science, Vol 4, Iss 1, Pp 1-8 (2021)
op_relation https://doi.org/10.1038/s41612-021-00177-8
https://doaj.org/toc/2397-3722
doi:10.1038/s41612-021-00177-8
2397-3722
https://doaj.org/article/96e2c3bf8c0f4d6787701274dcf87ec5
op_doi https://doi.org/10.1038/s41612-021-00177-8
container_title npj Climate and Atmospheric Science
container_volume 4
container_issue 1
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