More-persistent weak stratospheric polar vortex states linked to cold extremes

Kretschmer, M. ORCID: https://orcid.org/0000-0002-2756-9526, Coumou, D., Agel, L., Barlow, M., Tziperman, E. and Cohen, J. (2018) More-persistent weak stratospheric polar vortex states linked to cold extremes. Bulletin of the American Meteorological Society, 99 (1). pp. 49-60. ISSN 1520-0477 doi: 10.1175/BAMS-D-16-0259.1

Abstract/Summary

The extratropical stratosphere in boreal winter is characterized by a strong circumpolar westerly jet, confining the coldest temperatures at high latitudes. The jet, referred to as the stratospheric polar vortex, is predominantly zonal and centered around the pole; however, it does exhibit large variability in wind speed and location. Previous studies showed that a weak stratospheric polar vortex can lead to cold-air outbreaks in the midlatitudes, but the exact relationships and mechanisms are unclear. Particularly, it is unclear whether stratospheric variability has contributed to the observed anomalous cooling trends in midlatitude Eurasia. Using hierarchical clustering, we show that over the last 37 years, the frequency of weak vortex states in mid- to late winter (January and February) has increased, which was accompanied by subsequent cold extremes in midlatitude Eurasia. For this region, 60% of the observed cooling in the era of Arctic amplification, that is, since 1990, can be explained by the increased frequency of weak stratospheric polar vortex states, a number that increases to almost 80% when El Niño–Southern Oscillation (ENSO) variability is included as well.

Item Type	Article
URI	https://reading-clone.eprints-hosting.org/id/eprint/92432
Item Type	Article
Refereed	Yes
Divisions	No Reading authors. Back catalogue items
Publisher	American Meteorological Society
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