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  The North Atlantic jet stream: a look at preferred positions, paths and transitions

Hannachi, A., Woollings, T., & Fraedrich, K. (2012). The North Atlantic jet stream: a look at preferred positions, paths and transitions. Quarterly Journal of the Royal Meteorological Society, 138(665), 862-877. doi:10.1002/qj.959.

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 Creators:
Hannachi, A.1, Author
Woollings, T.1, Author
Fraedrich, K.2, Author           
Affiliations:
1external, ou_persistent22              
2The CliSAP Cluster of Excellence, External Organizations, Bundesstraße 53, 20146 Hamburg, DE, ou_1832285              

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Free keywords: EMPIRICAL ORTHOGONAL FUNCTIONS; QUASI-BIENNIAL OSCILLATION; EDDY-DRIVEN JET; HEMISPHERE WINTER; CLUSTER-ANALYSIS; INTERANNUAL VARIABILITY; CIRCULATION REGIMES; PLANETARY-WAVES; EOF ANALYSIS; BLOCKINGjet stream; circulation patterns; Greenland blocking; preferred paths; transition probability;
 Abstract: Preferred jet stream positions and their link to regional circulation patterns over the winter North Atlantic/European sector are investigated to corroborate findings of multimodal behaviour of the jet positions and to analyse patterns of preferred paths and transition probabilities between jet regimes using ERA-40 data. Besides the multivariate Gaussian mixture model, hierarchical clustering and data image techniques are used for this purpose. The different approaches all yield circulation patterns that correspond to the preferred jet regimes, namely the southern, central and the northern positions associated respectively with the Greenland anticyclone or blocking, and two opposite phases of an East Atlantic-like flow pattern. Growth and decay patterns as well as preferred paths of the system trajectory are studied using the mixture model within the delay space. The analysis shows that the most preferred paths are associated with central to north and north to south jet stream transitions with a typical time-scale of about 5 days, and with life cycles of 12 weeks. The transition paths are found to be consistent with transition probabilities. The analysis also shows that wave breaking seems to be the dominant mechanism behind Greenland blocking. Copyright (c) 2011 Royal Meteorological Society

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Language(s): eng - English
 Dates: 2012-04
 Publication Status: Issued
 Pages: -
 Publishing info: -
 Table of Contents: -
 Rev. Type: Peer
 Identifiers: ISI: 000305073200002
DOI: 10.1002/qj.959
 Degree: -

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Title: Quarterly Journal of the Royal Meteorological Society
Source Genre: Journal
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Pages: - Volume / Issue: 138 (665) Sequence Number: - Start / End Page: 862 - 877 Identifier: ISSN: 0035-9009
CoNE: https://pure.mpg.de/cone/journals/resource/954925442598