Rossby wave breaking, the upper level jet, and serial clustering of extratropical cyclones in western Europe

Priestley, M. D. K., Pinto, J. G., Dacre, H. F. ORCID: https://orcid.org/0000-0003-4328-9126 and Shaffrey, L. C. ORCID: https://orcid.org/0000-0003-2696-752X (2017) Rossby wave breaking, the upper level jet, and serial clustering of extratropical cyclones in western Europe. Geophysical Research Letters, 44 (1). pp. 514-521. ISSN 0094-8276 doi: 10.1002/2016GL071277

Abstract/Summary

Winter 2013/14 was the stormiest on record for the UK and was characterized by recurrent clustering of extratropical cyclones. This clustering was associated with a strong, straight and persistent North Atlantic jet and was also associated with Rossby wave breaking (RWB) on both flanks, pinning the jet in place. The occurrence of RWB and cyclone clustering is further studied in 36 years of the ERA-Interim Reanalysis. Clustering at 55°N is associated with an extended and anomalously strong eddy-driven jet flanked on both sides by RWB. However, clustering at 65(45)°N has a dominance of RWB to the south (north) of the jet, deflecting the jet northward (southward). A positive correlation was found between clustering and RWB occurrence to the north and south of the jet. However, there is considerable spread in these relationships.

Item Type	Article
URI	https://reading-clone.eprints-hosting.org/id/eprint/68986
Identification Number/DOI	10.1002/2016GL071277
Refereed	Yes
Divisions	Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Publisher	American Geophysical Union
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