Do CMIP5 models reproduce observed low-frequency North Atlantic jet variability?

The magnitude of observed multi-decadal variations in the North Atlantic Oscillation (NAO) is at the upper end of the range simulated by climate models and a clear explanation for this remains elusive. Recent research shows that observed multi-decadal NAO variability is more strongly associated with...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Woollings, T, Bracegirdle, T, Lu, H, Eade, R
Format: Article in Journal/Newspaper
Language:unknown
Published: John Wiley & Sons, Inc. 2018
Subjects:
Online Access:https://doi.org/10.1029/2018GL078965
https://ora.ox.ac.uk/objects/uuid:944a2013-f342-47c4-99a3-1a9c9a015b23
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Summary:The magnitude of observed multi-decadal variations in the North Atlantic Oscillation (NAO) is at the upper end of the range simulated by climate models and a clear explanation for this remains elusive. Recent research shows that observed multi-decadal NAO variability is more strongly associated with North Atlantic (NA) jet strength than latitude, thus motivating a comprehensive comparison of NA jet and NAO variability across the CMIP5 models. Our results show that the observed peak in multi-decadal jet strength variability is even more unusual than NAO variability when compared to the model-simulated range across 133 historical CMIP5 simulations. Some CMIP5 models appear capable of reproducing the observed low-frequency peak in jet strength, but there are too few simulations of each model to clearly identify which. It is also found that an observed strong multi-decadal correlation between jet strength and NAO since the mid-19th century may be specific to this period.